Relevant bibliographies by topics / Tarim, Bassin du (Chine)

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  2. Dissertations / Theses
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  4. Book chapters
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Academic literature on the topic 'Tarim, Bassin du (Chine)'

Author: Grafiati
Published: 4 June 2021
Last updated: 17 February 2022

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Journal articles on the topic "Tarim, Bassin du (Chine)"

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Chang, Hong, Zhisheng An, Weiguo Liu, et al. "Quaternary structural partitioning within the rigid Tarim plate inferred from magnetostratigraphy and sedimentation rate in the eastern Tarim Basin in China." Quaternary Research 81, no. 3 (2014): 424–32. http://dx.doi.org/10.1016/j.yqres.2013.10.018.

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AbstractIt has been proposed that within the Tarim Basin tectonic activity has been limited since Triassic time. However, on the basis of magnetostratigraphy from the eastern Tarim Basin, which defines the chronology of sedimentation and structural evolution of the basin, we show that the basin interior has been uplifted and partitioned during Quaternary. The magnetostratigraphy was constructed from 2228 samples that yielded acceptable inclination values. Characteristic remnant magnetization (ChRM) with both normal (N1–N11) and reversed (R1–R11) polarity was isolated by thermal demagnetization. The data correlate best with polarity chrons C3r to C1n, which range from 5.39 Ma to recent on the geological time scale 2004 (GTS2004). An abrupt decrease in the sedimentation rate is observed at 1.77 Ma in the Ls1 core. This change does not overlap with known Pleistocene climate-change events. We attribute this sedimentation rate decrease to a structurally controlled local decrease in accommodation space where basin basement uplifts occur. This period of sedimentary environmental change reveals that structural partitioning in the basement of the Tarim Basin occurred since ~ 1.77 Ma, and we speculate that tilting of the Southeast Uplift (a sub-basin unit) within the Tarim Basin began in early Pleistocene time.
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Xiao, Xianming, Zhiguang Song, Dehan Liu, Zufa Liu, and Jiamu Fu. "The Tazhong hybrid petroleum system, Tarim Basin, China." Marine and Petroleum Geology 17, no. 1 (2000): 1–12. http://dx.doi.org/10.1016/s0264-8172(99)00050-1.

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Huafu, Lu, David G. Howell, Jia Dong, et al. "Kalpin Transpression Tectonics, Northwestern Tarim Basin, Western China." International Geology Review 36, no. 10 (1994): 975–81. http://dx.doi.org/10.1080/00206819409465499.

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Lü, Xiuxiang, Yiwei Zhang, and Zhijun Jin. "Reservoir formation cycle of Tarim Basin, NW China." Chinese Science Bulletin 42, no. 3 (1997): 245–48. http://dx.doi.org/10.1007/bf02882447.

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Xiao, Zong Lin, Qing Qing Hao, and Zhong Min Shen. "Geotemperature Evolution of the Ordovician Strata in the Tarim Basin and its Petroleum Geology Significance." Advanced Materials Research 622-623 (December 2012): 1638–41. http://dx.doi.org/10.4028/www.scientific.net/amr.622-623.1638.

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The Tarim basin is an important petroleum basin in China, which produces a large amount of oil and gas resources. This paper calculates the geotemperature of the middle-upper Ordovician basal boundary during the main geological periods using the one-dimensional steady-state heat conduction equation. The simulation result reveals that from the late Ordovician to the present, the Manjiaer sag in the Tabei depression retains the highest temperature in the Tarim basin, and its highest temperature reaches 400°C in the present, while other areas in the Tarim basin have undergone relatively low temperature. Only in the Manjiaer sag of the Tabei depression and the Yecheng and Tanggubasi sags in the Southwest depression, the temperature exceeds 250°C, reaching the condition of liquid oil cracking into gas. Geotemperature of the middle-upper Ordovician basal boundary in the Tahe oilfield of the Central uplift is lower than 250 °C. It is thus inferred that there are abundant oil resources in the Ordovician strata of the Tahe oilfield. This study may provide effective geotemperature data for the next petroleum exploration in the Tarim basin.
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Zhao, Yong, Anning Huang, Yang Zhou, et al. "Impact of the Middle and Upper Tropospheric Cooling over Central Asia on the Summer Rainfall in the Tarim Basin, China." Journal of Climate 27, no. 12 (2014): 4721–32. http://dx.doi.org/10.1175/jcli-d-13-00456.1.

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Abstract The changes in summer rainfall over the Tarim Basin, China, and the underlying mechanisms have been investigated using the observed rainfall data at 34 stations and the NCEP–NCAR reanalysis data during the period of 1961–2007. Results show that the summer rainfall over the Tarim Basin, which exhibits a significant increasing trend during the last half century, is closely related to the summer middle and upper tropospheric cooling over central Asia. Mechanism analysis indicates that the middle and upper tropospheric cooling over central Asia results in a location farther south of the subtropical westerly jet over western and central Asia with anomalous southerly wind at lower levels and ascending motion prevailing over the Tarim Basin. Such anomalies in the atmospheric circulations provide favorable conditions for the enhanced summer rainfall over the Tarim Basin. Further analysis suggests that the weakened South Asian summer monsoon (SASM) could be potentially responsible for the middle and upper tropospheric cooling over central Asia. This is largely through the atmospheric responses to the diabatic heating effect of the SASM. A weakened SASM can result in an anomalous cyclone in the middle and upper troposphere over central Asia. The western part of the anomalous cyclone produces more cold air advection, which leads to the cooling. This study suggests indirect but important effects of the SASM on the summer rainfall over the Tarim Basin.
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Thevs, Niels. "Water Scarcity and Allocation in the Tarim Basin: Decision Structures and Adaptations on the Local Level." Journal of Current Chinese Affairs 40, no. 3 (2011): 113–37. http://dx.doi.org/10.1177/186810261104000305.

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The Tarim River is the major water source for all kinds of human activities and for the natural ecosystems in the Tarim Basin, Xinjiang, China. The major water consumer is irrigation agriculture, mainly cotton. As the area under irrigation has been increasing ever since the 1950s, the lower and middle reaches of the Tarim are suffering from a water shortage. Within the framework of the Water Law and two World Bank projects, the Tarim River Basin Water Resource Commission was founded in 1997 in order to foster integrated water resource management along the Tarim River. Water quotas were fixed for the water utilization along the upstream and downstream river stretches. Furthermore, along each river stretch, quotas were set for water withdrawal by agriculture and industry and the amount of water to remain for the natural ecosystems (environmental flow). Furthermore, huge investments were undertaken in order to increase irrigation effectiveness and restore the lower reaches of the Tarim River. Still, a regular water supply for water consumers along the Tarim River cannot be ensured. This paper thus introduces the hydrology of the Tarim River and its impacts on land use and natural ecosystems along its banks. The water administration in the Tarim Basin and the water allocation plan are elaborated upon, and the current water supply situation is discussed. Finally, the adaptations made due to issues of water allocation and water scarcity on the farm level are investigated and discussed.
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Xu, Xi, Andrew V. Zuza, An Yin, Xiubin Lin, Hanlin Chen, and Shufeng Yang. "Permian plume-strengthened Tarim lithosphere controls the Cenozoic deformation pattern of the Himalayan-Tibetan orogen." Geology 49, no. 1 (2020): 96–100. http://dx.doi.org/10.1130/g47961.1.

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Abstract The high strength of the Tarim Basin (northwestern China) lithosphere, widely regarded as a Precambrian craton, is evidenced by its resistance to Cenozoic deformation in the Himalayan-Tibetan orogen. However, Neoproterozoic suturing and early Paleozoic shortening within the Tarim Basin suggest that its rigidity is a relatively recent phenomenon with unknown cause. We reprocessed high-resolution magnetic data that show a 300–400-km-diameter radial pattern of linear anomalies emanating from a central region characterized by mixed positive-negative anomalies. We suggest that this pattern was generated by the previously hypothesized Permian (ca. 300–270 Ma) plume beneath the Tarim Basin. Constrained by published geochemical and geochronological data from plume-related igneous rocks, we propose that the ∼30 m.y. Permian plume activity resulted in a more viscous, depleted, thicker, dehydrated, and low-density mantle lithosphere. The resulting stronger lithosphere deflected strain from the Cenozoic India-Asia convergence around Tarim Basin, including Pamir overthrusting to the northwest and Altyn Tagh left-slip displacement to the northeast, thus shaping the geometry of the Himalayan-Tibetan orogen.
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Gao, Guoming, Guofa Kang, Guangquan Li, and Chunhua Bai. "Crustal magnetic anomaly and Curie surface beneath Tarim Basin, China, and its adjacent area." Canadian Journal of Earth Sciences 52, no. 6 (2015): 357–67. http://dx.doi.org/10.1139/cjes-2014-0204.

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Based on the geomagnetic field model NGDC-720-V3 (National Geophysical Data Center), the distribution of crustal magnetic anomalies and the Curie surface beneath Tarim Basin, China, and its adjacent area were investigated. The results show that the spatial distribution of the magnetic anomalies in Tarim Basin coincides with the regional tectonic structure, i.e., a basin sandwiched between mountain ranges. Shallow parts of the Curie surface are located in uplifted zones of the basin and correspond well to high values of heat flow. In contrast, deep parts of the Curie surface, having low values of heat flow, are distributed along the depression zones of the basin. The Curie point depth is consistent with the measured heat flow value, with a correlation coefficient of 0.65.
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Skjærvø, P. O. "On the Tumshuqese Karmavācanā text." Journal of the Royal Asiatic Society of Great Britain & Ireland 119, no. 1 (1987): 77–90. http://dx.doi.org/10.1017/s0035869x00166985.

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Tumshuqese is the name proposed by Emmerick, on the analogy of “Khotan: Khotanese”, for the language spoken in the region of Tumshuq, on the northern edge of the Tarim basin in the Xinjiang Uigur Autonomous Region of China. It is closely related to — though in many respects more archaic than — Khotanese, a Middle Iranian language (like Sogdian, Bactrian, Khwarezmian, Middle Persian and Parthian), the language of Khotan, a country and city on the southern border of the Tarim basin (see, e.g. Emmerick, 1979, 1–5).
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Dissertations / Theses on the topic "Tarim, Bassin du (Chine)"

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Shen, Yuefeng. "Les systèmes biosédimentaires et la diagénèse d'une rampe carbonatée Ordovicienne, Bassin de Tarim, Chine." Doctoral thesis, Université Laval, 2017. http://hdl.handle.net/20.500.11794/36433.

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L'enregistrement biosédimentaire Ordovicien du bassin de Tarim offre la possibilité de s'attaquer à quatre grands enjeux scientifiques liés au «grand événement de biodiversité ordovicienne » (Great Ordovician Biodiversification Event ou GOBE en anglais): i) la phylogenèse des organismes incertae sedis, ii) la paléodiversité des producteurs primaires benthiques (algues calcaires, calcimicrobes), iii) la nature des précipités authigénique des fonds marins (automicrite), et iv) la diagénèse en termes d'évolution de la porosité et de l'enregistrement géochimique des perturbations environnementales provoquant des changements biosédimentaires majeures (éponges, crinoïdes contre algues benthiques). L'analyse typologique, morphométrique et microstructurale du microfossile problématique Halysis Høeg, 1932, conclut pour une algue verte siphonnée avec une affinité à Bryopsidales, Udoteaceae, morphotype Flabellia petiolata (Turra) Nizamuddin 1987. Les monticules d’Halysis (Katian) font partie d'une rampe carbonatée peu profonde et subtidale dominée par des tapis de sable de granules d'algues. L’accrétion de monticules était contrôlée par des phénomènes autocycliques, produisant des épisodes sédimentaires et d’enfouissement suivis de lacunes et de périodes de croissance d’algue. Dans le bassin de Tarim, la diversité des producteurs primaires benthiques augmente considérablement au cours de la zone de Belodina confluens d’Ordovicien supérieur (Katian). Par rapport aux courbes de diversité dérivées d'autres régions (Laurentia, Baltoscandia), dans le bassin de Tarim, il y a une propagation de la diversification d'environ 4 Ma. La courbe de diversité des producteurs primaires benthiques sont semblables à celles enregistrées par certains groupes de fossiles herbivores et suspensivores (Échinodermes eleuthérozoaires, gastéropodes). Cinq types de précipitations authigénique des fonds marins (automicrite) sont présents dans les monticules carbonatés de calathid-demosponge (Darriwilian), tout d'abord interprété comme « carbonate microbien ». Une bonne corrélation de la fluorescence et de la cathodoluminescence des automicrites indique que l'organominéralisation induite et soutenue a produit de l'automicrite, probablement par la perminéralisation de substrats organiques non vivants adsorbant des complexes métal-humâtes dissous. À l'aide de six paramètres et de dix-sept caractères, quatre automicrites se révèlent non microbiennes au lieu de représenter probablement des reliques de métazoaires calcifiés (éponges, structures d'attachement des invertébrés tendus). Un automicrite est d'origine microbienne, mais l'âge de l'après-monticule réussit une disconformité. En utilisant un ensemble de séquences paragénétiques, un échantillonnage géochimique des composants spécifiques a été effectué pour déterminer la variation de la composition isotopique stable au carbone et à l'oxygène. Il existe deux niveaux stratigraphiques distincts séparés par Δδ13C ≈ +2.5 ‰ (PDB). Les deux niveaux suivent la même tendance partielle de diminution de δ18O typique pour l’augmentation de la température pendant l'enfouissement. Les valeurs de δ18O les moins modifiées sont également séparées selon les mêmes deux niveaux stratigraphiques (Δδ18O ≈ +2.0 ‰). Cette excursion positive couplée de δ13C-δ18O est considérée comme le résultat d'une augmentation du taux d'enfouissement du carbone organique (formation de roches mères d'hydrocarbures) et d'un refroidissement climatique subséquent provoquant un changement biosédimentaire majeure (éponges, crinoïdes contre algues benthiques) le long de l'intervalle limite Sandbian-Katian<br>The Ordovician biosedimentary record of the Tarim Basin offers the opportunity to tackle four major scientific issues related to the Great Ordovician Biodiversification Event: i) the phylogenesis of organisms incertae sedis, ii) the paleodiversity of benthic primary producers (calcareous algae, calcimicrobes), iii) the nature of authigenic sea-floor precipitates (automicrite), and iv) diagenesis in terms of porosity evolution and the geochemical record of environmental perturbations causing major biosedimentary turnovers (sponges, crinoids versusbenthic algae). The typological, morphometric and microstructural analysis of the mound-forming microproblematicum Halysis Høeg, 1932 concludes for a siphonous green alga with an affinity to Bryopsidales, Udoteaceae, morphotype Flabellia petiolate (Turra) Nizamuddin 1987. Early Katian Halysismounds form part of a shallow-subtidal carbonate ramp dominated by algal-pellet sand sheets. Their accretion was controlled by autocyclic drivers such as increments of sediment flux and burial followed by episodes of omission and algal growth. In the Tarim Basin, the diversity of benthic primary producers increases substantially during the Upper Ordovician (Katian) Belodina confluens Zone. Compared to diversity curves derived from other regions (Laurentia, Baltoscandia), in the Tarim Basin there is a protraction of diversification by about 4 Ma. The global diversity curve of benthic primary producers is similar to those derived from some herbivorous and suspension-feeding fossil groups (eleutherozoan echinoderms, gastropods). Five kinds of authigenic sea-floor precipitates (automicrite) are present in Darriwilian calathid-demosponge carbonate mounds, altogether formerly interpreted as ‘microbial carbonate’. A good correlation of fluorescence and cathodoluminescence of automicrites indicates that induced and supported organomineralization produced automicrite, probably via the permineralization of non-living organic substrates adsorbing dissolved metal-humate complexes. Using six parameters and seventeen characters, four automicrites turn out to be non-microbial instead likely represent relics of calcified metazoan tissue (sponges, attachment structures of stalked invertebrates). One automicrite is microbial in origin but is post-mound in age succeeding a disconformity. Using a set of paragenetic sequences, component-specific geochemical sampling was performed to determine the variation of carbon and oxygen stable isotopic composition. There are two distinct stratigraphic levels separated by Δδ13C ≈ +2.5‰ (PDB).Both levels display a subparallel trend of decreasing δ18O typical for increasing temperature during burial. Least altered δ18O values are equally separated along the two stratigraphic levels (Δδ18O ≈ +2.0‰). This coupled positive δ13C-δ18O excursion is considered the result of an increasing burial rate of organic carbon (formation of hydrocarbon source rocks) and subsequent climatic cooling causing a biosedimentary turnover (sponges, crinoids versusbenthic algae) along the Sandbian-Katian boundary interval.
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Zhan, Sheng. "Etudes paléomagnétiques du Néoprotozoïque du bassin du Nord du Tarim (Chine du Nord-ouest) et leurs implications géodynamiques." Orléans, 2007. http://www.theses.fr/2007ORLE2043.

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Au néo-protérozoïque, les deux questions fondamentales que sont la reconstruction du super-continent Rodinia et l'existence d'une glaciation globale restent un sujet de débat. Ces dernières années, l'hypothèse de la "snowball Earth" a été proposée pour expliquer la présence de glaciers à de basses latitudes pendant le néo-protérozoïque. Seules les données paléomagnétiques peuvent apporter la preuve de la présence de tel ou tel continent à basse latitude durant la période de glaciation globale. Par ailleurs, la reconstruction paléogéographique du super-continent Rodinia est très discutée par manque de données paléomagnétiques fiables en raison de la fréquente remagnétisation des séries sédimentaires anciennes. Parmi les blocs continentaux dont l'assemblage constituait la Rodinia le Tarim est le plus mal connu; par conséquent, en vue de résoudre les deux questions ci-dessus, l'acquisition de données paléomagnétiques de haute qualité a été effectuée au Tarim, en Chine du nord-ouest. Environ 450 carottes ont été collectées sur 60 sites de la région d'Aksu, au nord-ouest du Tarim, et environ 400 carottes ont été prélevées sur 52 sites de la région de Quruqtagh, au nord-est du Tarim. Vingt-quatre sites de grès et de roches volcaniques de la formation de Sugetbrak dans la région d'Aksu ont montré une rémanence magnétique stable avec des températures de Curie (ChRm) situées entre 500 et 680°C. Les directions magnétiques calculées à l'aide de ces composantes sont significativement différentes de celles des formations plus récentes; ce qui exclut une ré-aimantation. Des polarités normales et inverses ont été isolées, et un test du pli positif a été obtenu avec un niveau de confiance de 95%. L'anisotropie des mesures de susceptibilité magnétique montre que la structure sédimentaire est primaire avec un faible degré d'anisotropie. Un pôlepaléomagnétique aétéotenu à 19. 1°N, 149. 7°E, k= 11. 2, A95 = 9. 3° avecn = 24, ce qui correspond à une paleolatitude de -27°N pour le secteur de prélèvement. La datation chemo-stratigraphique de cette section indique un âge néo-protérozoïque de -595 Ma. Sept sites de calcaires de la formation de Tereeken dans la région de Quruqtagh ont donné une rémanence magnétique stable avec des températures de Curie (ChRm) situées entre 400 et 580°C. Les directions magnétiques calculées à l'aide de ces composantes sont significativement différentes de celles des formations plus récentes; ce qui exclut également une ré-aimantation. On distingue deux types de porteurs de la rémanence magnétique stable, les uns à haute température clairement distinct de ceux de basse température. L'AMS et l'étude du magnétisme des roches montrent que la rémanence magnétique dans les régions d'Aksu et de Quruqtagh est primaire. Par conséquent, un nouveau pôle paléomagnétique a été calculé à 31. 2DN, 135. 5°E, Dp=13. 6, Dm =11. 3°, défmissant une paléo-Iatitude de 50. 8°±13. 6°N. L'âge de la rémanence magnétique est calé sur la fin de la glaciation à 635 Ma connu par ailleurs et marqué localement par les calcaires de la formation de Tereeken. Une nouvelle reconstruction paléogéographique vers 600 Ma a été tentée montrant que les blocs Australie, Chine du sud et Tarim se situent à de basses latitudes. Le Tarim se situe au nord de l'Australie après l'arrêt de la glaciation de Marinien, cette observation fournit de nouvelles évidences pour l'hypothèse de Snowball. En utilisant les deux pôles paléomagnétiques fiables obtenus dans cette étude, et en les combinant avec les résultats paléomagnétiques disponibles dans la littérature, une courbe de dérive apparente (APWP) du pôle magnétique a été construite pour le bloc du Tarim du néo-protérozoïque à l'actuel. Vers 800-750 Ma, le Rodinia occidental qui comprenait l'Australie, l'Antarctique, le Tarim, la Chine du sud et l'Inde se sépare du supercontinent Rodinia. Ce bloc subit alors deux glaciations globales successives (750 et 635 Ma). Après l'arrêt de la glaciation du Marinien (635-520 Ma), il se déplace rapidement vers le sud. Au cambrien (600-550 Ma), le Tarim ainsi que l'Afrique et l'Amérique du sud se séparent du Rodinia occidental pour former le Gondwana. Le continent de Gondwana se déplace ensuite vers le nord entre 520 et 420 Ma. Le Tarim se situe alors au nord du Gondwana pour finalement s'en séparer au silurien. Si l'on compare les courbes de dérive du Tarim, de l'Australie et de la Chine du sud dans l'intervalle 785-420 Ma, on constate que ces trois blocs ont suivi la même trajectoire du néo-protérozoïque jusqu'au silurien supérieur.
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Yang, Wei. "L'évolution tectonique des chaînes du Tian Shan et Kunlun Shan occidentale contrainte par analyses magnétostratigraphiques et thermochronologiques." Thesis, Rennes 1, 2014. http://www.theses.fr/2014REN1S029/document.

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Deux questions scientifiques critiques sont adressées dans cette thèse présentées comme suit. ( 1 ) L’évolution mésozoïque du bassin d’avant-pays dans les piémonts nord et sud du Tian Shan. ( 2 ) L’évolution au Cénozoïque précoce du soulèvement du Tian Shan. Dans le chapitre 1, l'évolution du nord Tian Shan est étudiée par datation U/Pb (LA- ICP-MS) de zircons détritiques sur 14 échantillons de grès d'une série continue d’âge fin Paléozoïque à Quaternaire dans la marge sud du bassin de Junggar (région de Manasi). Dans le chapitre 2, l'évolution encore mal contrainte entre le Mésozoïque et le début du Cénozoïque de la marge sud-ouest du Tian Shan est étudiée en utilisant les datations U/Pb ( LA- ICP-MS ) sur zircons détritiques et les traces de fission sur apatites détritiques. Dans le chapitre 3, nous présentons une étude magnétostratigraphique détaillée de la zone Ulugqat au sud-ouest du Tian Shan, dans le but d'améliorer la compréhension de son soulèvement et de l'histoire de la déformation de la région au cours du Cénozoïque. Ce travail à permis de montrer que l'érosion du paléo-Tian Shan commencée au Trias moyen s’est traduite par le pénéplanation générale au Mésozoïque du Tian Shan qui était dominé par un système de drainage large pendant une longue période de quiescence tectonique. Le piémont nord du Tian Shan était caractérisé par un bassin en subsidence thermique post- extensive avec peu d'activité tectonique, et le piémont sud a également connu un aplanissement général de la topographie. Au cours du début du Jurassique, du Crétacé inférieur et du Crétacé supérieur, trois inversions tectoniques mineures sont identifiées avec des ajustements du bassin d’avant-pays du Tian Shan. Ces inversions peuvent correspondre respectivement à l’accrétion des terrains Cimmérien, de Lhassa, et du Kohistan-Dras à la limite sud de la plaque eurasienne. Les données U-Pb sur zircons détritiques et les données traces de fission sur apatite indiquent une première réorganisation du bassin à la fin du Crétacé – début du tertiaire, contemporaine d’une réactivation de l’érosion le long du piémont sud du Tian Shan. Nous avons interprété cette réactivation fin Crétacé – début Paléogène du Tian Shan sud à la réponse initiale des effets lointains de la collision Inde-Eurasie. Pendant le reste du Cénozoïque, la principale réactivation du Tian Shan est initiée fin Oligocène – début Miocène. Cela est attesté dans le piémont nord du Tian Shan par nos données U-Pb sur zircons détritiques et dans le piémont sud du Tian Shan par les données traces de fission sur apatite suggérant des chevauchements entre 18 et 16 Ma, par les résultats magnétostratigraphiques révélant une importante lacune de sédimentation oligocène ainsi que l’augmentation des taux d’accumulation à ~ 18.5 Ma<br>Two critical scientific issues are adressed in the présent thesis as follows. (1) Mesozoic basin-range relationship in the northern and southern piedmonts of the Tian Shan. (2) Spatio-temporal differences in the Early Cenozoic uplift of the Tian Shan. In chapter 1, the évolution of the northern Tian Shan is investigated through U/Pb (LA-ICP-MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary in the southern margin of the Junggar Basin (Manasi area). In chapter 2, the still poorly constrained Mezosoic to early Cenozoic evolution of the southwestern Tian Shan piedmont is investigated using U/Pb (LA-ICP-MS) dating of detrital zircons and fission track analysis on detrital apatites. In chapter 3, we present a detailed magnetostratigraphic study from the Ulugqat area in piedmont of the Southwest Tian Shan, in order to improve understanding of the uplift and deformation history of the Southwest Tian Shan during the Cenozoic. This work enabled to show that erosion of the Paleo-Tian Shan initiated in the Middle Triassic results in the general peneplanation of the Mesozoic Tian Shan dominated by a wide drainage system and long-lasting tectonic quiescence. The northern piedmont of the Tian Shan was characterized by a post-extensional thermally subsiding basin without much tectonic activity, and the southern piedmont also experienced a general flattening of topography. During the Early Jurassic, Early Cretaceous and Late Cretaceous, three identified minor tectonic inversions and adjustments of basin-range pattern in the Tian Shan, may potentially correspond respectively to the accretions of Cimmerian, Lhasa, and Kohistan-Dras in the southern margin of the Eurasian plate. Detrital zircon U-Pb and apatite fission-track data indicate an initial late Cretaceous – Early Tertiary basin reorganization and coeval renewed erosion along the southern Tian Shan piedmont. We interpreted this late Cretacesou to Paleogene activity in STS as the initial response of the distant effects of India-Eurasia collision as previously argued. During the Late Cenozoic, the major reactivation of the Tian Shan initiated around the Late Oligocene-Early Miocene times. This is evidenced mainly from the detrital zircon U-Pb geochronology in the northern piedmont of the Tian Shan, the apatite fission-track data suggesting a possible activation of the Talas Fergana Fault between 18 and 16 Ma, the major Oligocene depositional hiatus and conspicuous increase in accumulation rates at ~ 18.5 Ma revealed by the magnetostratigraphic results in the southern piedmont of the Tian Shan
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Guilbaud, Christelle. "Kinematics of active deformation of the Western Kunlun Range (Xinjiang, China) : implications for potential seismic hazards." Thesis, Université de Paris (2019-....), 2019. http://www.theses.fr/2019UNIP7112.

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La chaîne du Kunlun Occidental est une chaîne de montagnes intra-continentale en déformation lente, située à la bordure Nord-Ouest du plateau du Tibet. Malgré des évidences de raccourcissement au travers de la chaîne durant le Cénozoique, les taux de raccourcissement actuels sont trop faibles pour être quantifiés par les techniques géodésiques classiques. Par ailleurs, cette région n’a enregistré que peu de sismicité, mais le récent séisme de Pishan en juillet 2015 (Mw 6.4) atteste encore de son activité de nos jours. Dans cette thèse, nous cherchons à identifier les structures actives qui accommodent actuellement le raccourcissement, ainsi qu’à quantifier le taux de raccourcissement au travers de la chaîne, et à explorer la possibilité d’avoir de grands séismes dans cette région.Nous nous concentrons tout d’abord sur la zone épicentrale du séisme de Pishan. En combinant une analyse d’images satellites et de MNT, nous identifions neuf niveaux de terrasses fluviales et de surfaces alluviales incisées au niveau du pli de Yecheng-Pishan. Grâce à certains niveaux datés et à l’enregistrement de leur incision, nous quantifions le taux de raccourcissement sur cette structure à 0.5-2.5 mm/an sur les derniers 400 ka, avec une valeur long-terme plus probable entre 2-2.5 mm/an. A l’aide d’une étude structurale basée sur des cartes géologiques, données de terrain et profils de sismique réflexion du front de chaîne, nous identifions l'écaille chevauchante frontale formant le front de déformation de la chaîne du Kunlun Occidental. Cette écaille est enracinée dans un décollement superficiel, émergeant en surface au sein du bassin du Tarim, 150 à 180 km au nord du front morphologique de la chaîne, au niveau de la ride du Mazar Tagh. De telles dimensions impliquent la possibilité de grands séismes (M&gt;8) si ce décollement était actuellement bloqué et venait à rompre en une fois. Afin d'explorer la potentielle segmentation structurale et d’éventuelles variations du taux de raccourcissement le long du front de chaîne, une étude morpho-structurale du pli de Hotan, situé ~100 km à l'est de Pishan, est menée. Trois coupes géologiques sont réalisées au travers de cette structure, puis combinées avec l’analyse morphologique de terrasses fluviales. Ainsi, malgré des variations sur le nombre de structures aveugles accommodant la déformation active, le taux de raccourcissement semble similaire tout le long du front de chaîne. Ce scénario semble toutefois avoir été plus complexe dans le passé géologique. Enfin, pour avoir une meilleure compréhension de la façon dont la déformation est accommodée au travers de ce système de failles, et afin de vérifier la viabilité de la cinématique connectant le front de chaîne au Mazar Tagh, nous réalisons une nouvelle étude morpho-structurale de la zone où la rampe émerge en surface au cœur du bassin du Tarim. Une coupe géologique est construite à partir d’un profil sismique, permettant d’obtenir la géométrie précise de la rampe. Malgré l’aridité de la région, des terrasses ont été identifiées et échantillonnées pour datation OSL et 10Be. Ces terrasses sont ensuite cartographiées afin de quantifier la déformation enregistrée par ces marqueurs. Cette analyse nous permet ainsi de montrer que la déformation est bien transmise jusqu’à la rampe émergeant en surface au Mazar Tagh. Nous explorons ensuite le potentiel aléa sismique de la région en étudiant des marqueurs morphologiques qui pourraient avoir enregistré des séismes passés. Nos résultats apportent de ce fait une meilleure connaissance des structures actives et de la cinématique de la déformation dans cette chaîne de montagnes, et permettent de discuter du potentiel aléa sismique de la région<br>The Western Kunlun mountain range is a slowly converging intra-continental orogen located at the northwestern boundary of the Tibetan Plateau. Despite evidence of shortening through the range during the Cenozoic, present-day shortening rates are too low to be properly quantified from geodetic techniques. This region has also recorded limited seismicity, but the recent July 2015 (Mw 6.4) Pishan earthquake shows that this mountain range remains seismic. In this thesis, we aim at identifying the structures that actively accommodate this deformation across the range, at quantifying their slip rate and at exploring the potential for major earthquakes in this region.To do so, we first focus on the epicentral zone of the Pishan earthquake. Combining analysis of satellite images and DEMs, we obtain a detailed morphological analysis of the Yecheng-Pishan fold and find nine levels of incised fluvial terraces and alluvial fans. From their incision pattern and using age constraints available on some of these terraces, we are able to quantify the slip rate on the underlying blind frontal ramp to 0.5 to 2.5 mm/yr over the last ~400 kyr, with a most probable long-term value of ~2.0-2.5 mm/yr. Thanks to a structural study of the mountain front based on topographical and geological maps, field observations and available seismic profiles, we also identify a major active thrust sheet forming the deformation front of the Western Kunlun Range. This thrust sheet roots into a shallow decollement that emerges at the surface 150-180 km further north within the Tarim Basin, at the Mazar Tagh ridge. Such important dimensions imply the possibility of major M ≥ 8 earthquakes in the case that the whole decollement is presently seismically locked and fully ruptures in one single seismic event. With the idea of exploring potential along-strike structural segmentation or variations in deformation rate or in kinematics along the mountain front, a morpho-structural analysis is also conducted at the Hotan anticline, located ~100 km east of the Pishan epicentral area, along the morphological front of the Western Kunlun. Here, we build three geological cross- sections and investigate the record of preserved fluvial terraces. Despite a change in the number of active blind structures accommodating deformation, the slip rate remains similar along the mountain front. This pattern may however have been more complex in the geological past. Finally, to have a better understanding on how this deformation is accommodated through this fault system and to further test the possibility that the Mazar Tagh is really structurally and kinematically related to the folds of the mountain front, we conduct a new morphological and structural analysis of the most frontal ramp emerging at the Mazar Tagh ridge. A structural cross-section is built thanks to the combination of a seismic profile crossing the ridge and using field measurements, allowing us to get the precise geometry of the emerging ramp. Despite the current aridity of the region, a set of terraces is identified and sampled in the field for OSL and 10Be dating. Using Pléiades images and derived DEMs, we map theses terraces to quantify the amount of deformation recorded by these markers. This analysis shows that the kinematics proposed is viable and deformation is most reasonably transmitted from the topographic front of the Western Kunlun Range all the way to the Mazar Tagh emerging ramp. We also investigate potential geomorphic markers that may keep a record of past mega-earthquakes at this site of the deformation front. Our results help us get a better knowledge on the structure and kinematics of this range and its deformation front, and to discuss potential seismic hazards in this slowly deforming region
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Turner, Sebastian. "Structural evolution of the Northwest Tarim Basin, China." Thesis, Imperial College London, 2010. http://hdl.handle.net/10044/1/6213.

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The sedimentary and structural record of the NW Tarim Basin, China, provides an insight into the amalgamation of Central Asia and is an ideal area in which to examine the impact of an inherited tectonostratigraphic framework on the evolution of foreland fold-thrust belts. The NW Tarim Basin contains a thick (3-16 km) sedimentary succession which was deposited from the Late Neoproterozoic onwards, and has been exhumed by a foreland fold-thrust belt system associated with the South Tien Shan mountains during the Middle to Late Cenozoic. The research presented in this thesis combines satellite image interpretation and field investigations in order to examine the tectonostratigraphic framework of the NW Tarim Basin and to ascertain the causes of lateral structural variability and partitioning of the foreland fold-thrust belt system. The Upper Neoproterozoic to Lower Permian sedimentary succession records the progressive evolution of the NW Tarim Basin as a rift, intracratonic and foreland basin. Following a period of subaerial exposure throughout the Mesozoic, tectonic subsidence from the Middle Cenozoic onwards was driven by flexural deflection beneath the Pamirs and Tien Shan orogenic belts. This was coupled with the development of a foreland fold-thrust belt system along the northwest margin of the Tarim Basin. Lateral variations in the structural geometry, architecture and style of the foreland fold-thrust belt system correspond to changes in the thickness of the sedimentary succession and interaction with inherited, basement fault zones. An eastwest transition from the wide, arcuate Keping Shan Thrust Belt into the narrow Kashgar Fold Belt is ascribed to thickening of the Cenozoic (syn-tectonic) foreland basin succession. In contrast, internal variations in the structural architecture of the Keping Shan Thrust Belt are governed by lateral changes in the thickness of the Palaeozoic (pre-tectonic) sedimentary succession. These changes occur abruptly across inherited, Early Permian fault zones that have been reactivated as strike-slip faults in order to accommodate these lateral variations in the structure of the fold-thrust belt.
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Yang, Shenghong, and 杨胜洪. "The permian Pobei mafic-ultramafic intrusion (NE Tarim, NW China) and associated sulfide mineralization." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B45874219.

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Gao, Hang. "Dust variability and transport in China : a study of the Tarim basin." Thesis, University of Oxford, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.496451.

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Chen, Zhong Qiang, and mikewood@deakin edu au. "Late palaeozoic sequence stratigraphy and brachiopod faunas of the Tarim Basin, Northwest China." Deakin University. School of Ecology and Environment, 2001. http://tux.lib.deakin.edu.au./adt-VDU/public/adt-VDU20050915.141146.

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This thesis deals with the stratigraphy and brachiopod systematic palaeontology of the latest Devonian (Famennian) to Early Permian (Kungurian) sedimentary sequences of the Tarim Basin, NW China. Brachiopod faunas of latest Devonian and Carboniferous age have been published or currently in press in the course of the Ph.D candidature and are herein appendixed, while the Early Permian brachiopod faunas are systematically described in this thesis. The described Early Permian brachiopod faunas include 127 species, of which 29 are new and 12 indeterminate, and six new genera (subgenera) are proposed; Tarimella, Bmntonella, Marginifera (Arenaria), Marginifera (Nesiotia), Baliqliqia and Ustritskia. A new integrated brachiopod biostratigraphical zonation scheme is proposed, for the first time, for the latest Devonian-Early Permian sequences of the entire Tarim Basin on the basis of this study as well as previously published information (including the Candidate's own published papers). The scheme consists of twenty three brachiopod acm biozones, most of which replace previously proposed assemblage or assemblage zones. The age and distribution of these brachiopod zones within the Tarim Basin and their relationships with other important fossil groups are discussed. In terms of regional correlations and biostratigraphical affinities, the Late Devonian to Early Carboniferous brachiopod faunas of the Tarim Basin are closest to those from South China, while the Late Carboniferous faunas demonstrate strong similarities to coeval faunas from the Urals, central Asia, North China and South China. During the Asselian-Sakmarian, strong faunal links between the Tarim Basin and those of the Urals persisted, while at the same time links with central Asia, North China and South China weakened. On the other hand, during the Artinskian-Kungurian times, affinities of the Tarim faunas with the Urals/Russian Platform rapidly reduced, when those with peri-Gondwana (South Thailand, northern Tibet) and South China increased. Thirty lithofacies (or microfacies) types of four facies associations are recognised for the Late Devonian to early Permian sediments. Based on detailed lithostratigraphy, biostratigraphy and facies analysis, 23 third-order sequences belonging to four supcrsequences are identified for the Late Devonian to Early Permian successions, from which sea-level fluctuation curves are reconstructed. The sequence stratigraphical analysis reveals that four major regional regressions, each marking a distinct supersequence boundary, can be recognised; they correspond to the end-Serpukhovian, end-Moscovian, late Artinskian and end-Kungurian times, respectively. The development of these sequences is considered to have been formed and regulated by the interplay of both eustasy and tectonism. Using the system tract of a sequence as the mapping time unit, a succession of 47 palaeogeographical maps have been reconstructed through the Late Devonian to Early Permian. These maps reveal that the Tarim Basin was first immersed by southwest-directed (Recent geographical orientation) transgression in the late Famennian after the Caledonian Orogeny. Since then, the basin had maintained its geometry as a large, southwest-mouthed embayment until the late Moscovian when most areas were the uplifted above sea-level. The basin was flooded again in late Asselian-Artinskian times when a new transgression came from a large epicontinental sea lying to its northwest. Thereafter, marine deposition was restricted to local areas (southwestern and northwestern margins until the late Kungurian, while deposition of continental deposits prevailed and continued through the Middle and late Permian into the Triassic.
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Pla, de Casacuberta Oriol. "Salt tectonics in contractional fold belts, the Kuqa foreland basin and thrust belt case (Tarim basin, China)." Doctoral thesis, Universitat de Barcelona, 2019. http://hdl.handle.net/10803/668459.

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The thesis presented here spins off from the 2-year oil-industry project entitled “Salt Tectonics Modelling at Kuqa Foreland Fold and Thrust Belt, Tarim Oilfield” that was a collaboration between the American-based company China Petroleum Corporation (CNPC USA) and GEOMODELS Research Institute (via Fundació Bosch i Gimpera). This research project stems from the need to understand the structural character and evolution of the Kuqa fold- and-thrust belt (NW Xina) in order to identify exploration targets at the Mesozoic subsalt level. Specifically, the aim of the study was to identify exploration targets at the Paleogene subsalt structural level of the Kuqa foreland basin and adjoining fold and thrust belt, in particular beneath the Qiulitage fold-and-thrust system. In this scenario, the project research was focused on the definition and understanding of the different salt structures, their relationship with the geodynamic context and the different types of related hydrocarbon traps. To achieve these objectives, it was agreed to carry out six regional cross-sections, three of them balanced and restored as well as eleven balanced cross-sections of the Qiulitage fold-and-thrust system, three of them restored. In addition, regional structural maps were produced showing the salt and subsalt structures as well as their relationships with salt distribution and thickness. This line of research has been complemented with the realization of eight numerical discrete-element models and eight scaled sandbox analogue models of tectonic wedges incorporating variations in the rheology of a weak layer and in the syn- kinematic sedimentary rate. In order to accomplish these tasks, the company provided around 1500 km of 2D seismic lines and geophysical logs from numerous wells drilled in the area. In addition, two field campaigns were organized between June (15 days) and September 2015 (21 days) where structural data were collected to recognize the surface structure of the Kuqa fold-and-thrust belt. Moreover, several transects were realized during these field campaigns to recognize the surface expression of interpreted structures in the seismic lines. In this context, this thesis deals only with the results obtained from the structural analysis based on surface and subsurface data and analogue modelling. These results are presented in this manuscript which includes the following chapters. CHAPTER 1 that provides a summary of the thesis. CHAPTER 2 which provides a general introduction to the geology and the kinematic evolution of the Tian Shan intraplate range. Then, the chapter focuses in the southern frontal structure of the central Tian Shan Range, the Kuqa fold-and-thrust belt, describing both the stratigraphy and the main features of its structure. Finally, the main objectives of this thesis are presented. CHAPTER 3 that deals with the structural analysis carried out in the Kuqa fold-and- thrust belt with the field and subsurface data. The chapter shows the input data and the interpretation of both surface and subsurface data. The chapter describes the obtained results of three regional cross-sections as well as the regional structural maps of salt distribution and thickness. In addition, the chapter provides a kinematic evolution of the Kuqa fold-and-thrust belt and discusses the main parameters controlling it. CHAPTER 4 that describes the data, methodology, procedure and results obtained in the analogue modelling experiments. These experiments where designed to analyze the influence of the rheological properties of two superimposed décollement layers but mainly the one of the syn-tectonic sedimentation. So, after a brief introduction to the purpose of the experimental program and the methodology used, this chapter describes the experimental results separating them according to the applied syn-kinematic sedimentary rate. Then, the obtained results are compared and discussed mainly focusing on: the influence of the mechanical properties of a weak layer; the syn-kinematic sedimentary rate in the geometry and kinematics of brittle-viscous tectonic wedges; as well as the interaction between sub-salt and salt-detached structures. CHAPTER 5 which compares the experimental results with the structure and kinematic of the Kuqa fold-and-thrust belt defined from our structural field and subsurface analyses that is described in the Chapter 3. CHAPTER 6 which depicts the main conclusions of this thesis. CHAPTER 7 formed by the references mentioned throughout the text.<br>El cinturó de plecs i encavalcaments de Kuqa, situat a l’avantpaís meridional de la serralada del Tian Shan occidental, va ser deformat contractivament durant el Mesozoic superior i el Cenozoic tal com queda registrat a les seqüències sin-tectòniques continentals. A més a més, la seva evolució estructural va ser fortament controlada per la presència de sal sin- orogència (d’edat Eocè-Oligocè) i dels décollements pre-sal. En aquest context, presentem un conjunt de sis talls geològics, tres d’ells restituïts, a través del cinturó de plecs i encavalcaments de Kuqa que proporcionen una nova interpretació de la estructura per sota de les evaporites, en la qual els materials paleozoics i mesozoics estan deformats per un apilament d’encavalcaments involucrant (i) un sistema d’encavalcaments de pell fina desenganxats en nivells de carbó triàsics-juràssics, i (ii) un conjunt d’encavalcaments de basament de vergència nord. Les restitucions regionals mostren tres estadis evolutius pel cinturó de plecs i encavalcaments de Kuqa: i) una extensió mesozoica menor; ii) una compressió primerenca (Cretaci superior fins Miocè inferior) amb taxes d’escurçament i sedimentació baixes; i iii) un estadi de compressió tardana (Pliocè superior-Pleistocè) caracteritzat per un creixement major i progressiu de les taxes d’escurçament i sedimentació. Per tal d’esclarir la influència de la taxa de sedimentació, els canvis laterals en la reologia dels décollements, i la interacció entre décollements en l’estil de deformació de l’avantpaís de cinturons de plecs i encavalcaments presentem un estudi experimental que inclou quatre models analògics 3D inspirats en el cinturó de plecs i encavalcaments de Kuqa. Els resultats experimentals mostren que augmentant la taxa de sedimentació es retarda el desenvolupament d’estructures contractives frontals desenganxades a la sal, afavorint la formació i reactivació d’encavalcaments i retro-encavalcaments a les zones internes. El nostre estudi revela que a mesura que la viscositat del décollement pre-cinemàtic augmenta la deformació es propaga lentament cap a l’avantpaís. Per altre banda, les estructures sub-sal poden: (i) determinar la extensió areal de la sal i per tant l’extensió del cinturó de plecs i encavalcaments desenganxats en ell i, (ii) retardar o inclús prevenir la propagació de la deformació sobre el nivell salí cap a l’avantpaís.
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Aihemaitijiang, Rouzi [Verfasser], Bernd [Akademischer Betreuer] Cyffka, and Ümüt [Akademischer Betreuer] Halik. "Sustainable land use alternatives in the Tarim Basin, China / Rouzi Aihemaitijiang (Ahmatjan). Betreuer: Bernd Cyffka ; Ümüt Halik." Eichstätt-Ingolstadt : Katholische Universität Eichstätt-Ingolstadt, 2016. http://d-nb.info/1100055703/34.

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Books on the topic "Tarim, Bassin du (Chine)"

1

Jia, Chengzao. Tectonic characteristics and petroleum, Tarim Basin, China. Petroleum Industry Press, 1997.

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Talimu Pendi gou zao chen ji yu cheng cang: Talimupendigouzaochenjiyuchengcang. Di zhi chu ban she, 2010.

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Mao, Shaozhi. Late Cretaceous-early Tertiary dinoflagellates and acritarchs from the Kashi area, Tarim Basin, Xinjiang Province, China. Royal Ontario Museum, 1988.

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Talimu He liu yu qi hou bian hua ying xiang ping gu bao gao: China climate change impact report : Tarim River Basin. Qi xiang chu ban she, 2014.

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Associates, Gustavson, ed. The Petroleum geology and exploration potential of the Tarim Basin, China. Gustavson Associates, 1993.

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Geological Survey (U.S.), ed. Geology of the Tarim Basin with special emphasis on petroleum deposits, Xinjiang Uygur Zizhiqu, Northwest China. [U.S. Geological Survey], 1985.

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Book chapters on the topic "Tarim, Bassin du (Chine)"

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Ma, Yongsheng. "Progress and Theory of Marine Strata Oil and Gas Exploration in the Tarim Basin." In Marine Oil and Gas Exploration in China. Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-662-61147-0_17.

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Wu, Zhenyun, Hongwei Yin, and Hemin A. Koyi. "Compressional Salt-Related Structures in the Western Quele Area, Kuqa Depression, Tarim Basin, China." In Atlas of Structural Geological Interpretation from Seismic Images. John Wiley & Sons, Ltd, 2018. http://dx.doi.org/10.1002/9781119158332.ch30.

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Qin, Mingkuan, Wenming Dong, and Guangxi Ou. "Reduction of fluids in the Bashbulak sandstone type uranium deposit in the Tarim Basin, China." In Mineral Deposit Research: Meeting the Global Challenge. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_81.

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Cao, Peng, Zhan-feng Qiao, Guan-ming Shao, Jie Zhang, and Xiao-wei Sun. "Thin Low-Permeability Layers Characterization and Geological Modeling of YMX Dolomite Reservoir, Tarim Basin, China." In Springer Series in Geomechanics and Geoengineering. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-2485-1_1.

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Huang, Qingyu, Suyun Hu, Wei Liu, Tongshan Wang, and Congsheng Bian. "Origin and Preservation of Microbialite-Dominated Carbonate Reservoirs, Lower Cambrian Xiaoerbulake Formation, Tarim Basin (China)." In The Structural Geology Contribution to the Africa-Eurasia Geology: Basement and Reservoir Structure, Ore Mineralisation and Tectonic Modelling. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-01455-1_31.

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Liu, Jiangyu, Xuefang Yuan, Jian Zhang, Wang Xi, Jueyong Feng, and Hongjun Wu. "Sharp Reductions in High-Productivity Well Due to Formation Damage: Case Study in Tarim Basin, China." In Springer Series in Geomechanics and Geoengineering. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-7560-5_78.

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Pirajno, Franco. "Volcano-sedimentary and Sedimentary Basins in China: Junggar, Tarim, Tuha, Qaidam-Hoh Xil, Ordos; Basins in Eastern China Associated with Lithospheric Thinning (Songliao, Bohai)." In The Geology and Tectonic Settings of China's Mineral Deposits. Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4444-8_8.

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Liu, Jiang-yu, Jian Zhang, Ju Liu, Xuefang Yuan, Dengfeng Ren, and Yuan Liu. "Silicate Particles Produced During the Acidizing of a HTHP Tight Gas Reservoir in Tarim Basin, China: A Laboratory Study." In Springer Series in Geomechanics and Geoengineering. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-2485-1_42.

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Wang, Yijun, Yili Kang, Lijun You, Xiaopeng Yan, and Jiaxue Li. "Comprehensive Evaluation Method of Drill-in Fluid Damage in Fractured Tight Sandstone Gas Reservoir - A Case Study in the ZM Formation, Tarim Basin, China." In Springer Series in Geomechanics and Geoengineering. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-2485-1_54.

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"Petroleum Geology and Prospects of the Tarim (Talimu) Basin, China." In Giant Oil and Gas Fields of the Decade 1978-1988. American Association of Petroleum Geologists, 1992. http://dx.doi.org/10.1306/m54555c31.

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Conference papers on the topic "Tarim, Bassin du (Chine)"

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Guo, Ning, Huiwen Xie, Chao Wu, Anming Xu, Zhiyong Liu, and Zhibo Ma. "Challenges for Seismic Imaging in the Tarim Basin." In SEG/SINOPEC Foothill Technical Forum, Nanjing, China, 23-24 April 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/foothill2017-4.

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Zeng, Hongliu, Zhaohui Xu, Wei Liu, Qilong Fu, and Xavier Janson. "Seismic-informed carbonate shelf-to-basin transition in Cambrian, Tarim Basin, China." In SEG Technical Program Expanded Abstracts 2020. Society of Exploration Geophysicists, 2020. http://dx.doi.org/10.1190/segam2020-3424378.1.

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Sun, Changlong, Hongru Du, Xiaoliang Xu, Wenwen Ma, and Zhongsheng Chen. "Dynamic Variation of Economic Difference in Tarim Basin, Xinjiang, China." In 2010 International Conference on Challenges in Environmental Science and Computer Engineering. IEEE, 2010. http://dx.doi.org/10.1109/cesce.2010.267.

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Yang, P., Y. L. Liu, H. Y. Li, G. J. Dan, H. T. An, and Y. M. Shao. "Fractured-vuggy Reservoir Characterization of Carbonate, Tarim Basin, Northwest China." In 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011. EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20149450.

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Liu, Yimou, Yi Zhou, Xianghao Liang, Xueqiang Chen, and Naijian Wang. "Single-sensor field experiments in the Tarim basin, western China." In International Geophysical Conference, Beijing, China, 24-27 April 2018. Society of Exploration Geophysicists and Chinese Petroleum Society, 2018. http://dx.doi.org/10.1190/igc2018-024.

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Zhu, D. Y., Z. J. Jin, Q. Q. Meng, and Q. Y. Liu. "Deep Hydrothermal Altered Dolomite Reservoir in the Tarim Basin Northwestern China." In 75th EAGE Conference and Exhibition incorporating SPE EUROPEC 2013. EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20130683.

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Sun, Zhandong, Ni-Bin Chang, Christian Opp, and Thomas Hennig. "Spatial and temporal characteristics of aridity conditions in Tarim Basin, China." In Remote Sensing, edited by Ulrich Michel and Daniel L. Civco. SPIE, 2010. http://dx.doi.org/10.1117/12.864956.

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Hu, S. H., X. W. Wang, W. Q. Liu, and B. Zhang. "Seismic Numerical Simulating of Carbonate Caves in Tarim Basin, Western China." In 80th EAGE Conference and Exhibition 2018. EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201801654.

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Ping, Yang, Liu Yonglei, Hou Yunpeng, Jia Huiqing, Lü Dong, and Li Haiying. "Carbonate‐reservoirs prediction strategy and technologies in Tarim Basin of China." In SEG Technical Program Expanded Abstracts 2007. Society of Exploration Geophysicists, 2007. http://dx.doi.org/10.1190/1.2793035.

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Lu, Xinbian, Xinhua Li, Yuanshuai Rong, Chengjiang He, Zhihua Li, and Feng Shen. "Characterization of a Faulting Controlled Karst Reservoir in the Tarim Basin, China." In SPE Reservoir Characterisation and Simulation Conference and Exhibition. Society of Petroleum Engineers, 2015. http://dx.doi.org/10.2118/175660-ms.

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