Relevant bibliographies by topics / Tarim Basin

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Tarim Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 15 June 2025

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Journal articles on the topic "Tarim Basin"

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Norin, Erik. "Tertiary of the Tarim Basin*." Bulletin of the Geological Society of China 14, no. 3 (2009): 337–48. http://dx.doi.org/10.1111/j.1755-6724.1935.mp14003006.x.

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Chang, Haining, Guiting Hou, Shaoying Huang, et al. "Analysis of proto-type Tarim Basin in the late Precambrian and the dynamic mechanism of its evolution." PLOS ONE 18, no. 6 (2023): e0286849. http://dx.doi.org/10.1371/journal.pone.0286849.

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Tarim Basin has undergone an intricate tectonic evolution history ever since its formation from two discrete terranes in Neoproterozoic rather than in the Paleoproterozoic. More precisely, the amalgamation is assumed to happen during 1.0–0.8 Ga based on plate affinity. As the beginning of a unified Tarim block, studies of Tarim Basin in the Precambrian are basic and important. After the amalgamation of south and north paleo-Tarim terranes, Tarim block was experiencing a complicated tectonic process of being affected by mantle plume related to the breakup of Rodinia supercontinent in the south, and compressed by the Circum-Rodinia Subduction System in the north. The breakup of Rodinia supercontinent finished in the late Sinian Period, leading Kudi Ocean and Altyn Ocean to open and separating Tarim block from itself. According to the residual strata thickness, drilling data, and lithofacies distribution, the proto-type basin and tectono-paleogeographic maps of Tarim Basin in the late Nanhua Period and Sinian Period are reconstructed. With these maps, the characteristics of the rifts are revealed. Two rift systems were developed inside the unified Tarim Basin in the Nanhua Period and Sinian Period, one back-arc rift system in the northern margin and the other aulacogen system in the southern margin. The azimuth distribution of the rifts in Quruqtagh showed a predominant NE-SW trend, and the rifts in Aksu trended mainly NW-SE, while the rifts in Tiekelike trended SW-NE. With a three-dimensional elastic FEM (Finite Element Method) model that includes all rifts and deposited areas in Tarim Basin, applying the southern subduction and northern mantle upwelling properly to get the paleotectonic mian stress axes and the differential stress field, the dynamic mechanisms of rifts evolution are proved to be related to the peripheral tectonic environment mentioned above.
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Hai, H. E., and L. U. Guihua. "Precipitation Recycling in Tarim River Basin." Journal of Hydrologic Engineering 18, no. 11 (2013): 1549–56. http://dx.doi.org/10.1061/(asce)he.1943-5584.0000503.

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Chen, Hanlin, Shufeng Yang, Chuanwan Dong, et al. "Geological thermal events in Tarim Basin." Chinese Science Bulletin 42, no. 7 (1997): 580–84. http://dx.doi.org/10.1007/bf03182623.

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Li, Taohui, Aifeng Lv, Wenxiang Zhang, and Yonghao Liu. "Spatiotemporal Characteristics of Watershed Warming and Wetting: The Response to Atmospheric Circulation in Arid Areas of Northwest China." Atmosphere 14, no. 1 (2023): 151. http://dx.doi.org/10.3390/atmos14010151.

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The Tarim Basin is a large inland arid basin in the arid region of northwest China and has been experiencing significant “warming and wetting” since 1987. As a result, the purpose of this paper is to determine whether the climate transition phenomenon occurred in the Tarim Basin as well as the role of atmospheric circulation in this process. We use meteorological data and atmospheric circulation indexes to study the seasonal trends of climate change in this region from 1987 to 2020 to understand how they are affected by atmospheric circulation. The findings show that, from 1987 to 2020, the Tarim Basin experienced significant warming and wetting; with the exception of the winter scale, all other seasonal scales exhibited a clear warming and wetting trend. From the perspective of spatial distribution, most of the areas showed a significant warming trend, and the warming amplitude around the basin is greater than that in the central area of the basin. However, there are significant regional differences in precipitation change rates. Meanwhile, wavelet analysis shows that there is a significant oscillation period of 17–20 years between climate change and the atmospheric circulation index during 1987–2020. The correlation analysis shows that the Pacific decadal oscillation (PDO) and El Niño-Southern Oscillation (ENSO) are the main influencing factors of climate change in the Tarim Basin at different seasonal scales, while the teleconnection of the Arctic Oscillation (AO) and North Atlantic Oscillation (NAO) is low and the PDO dominates the summer and autumn temperature changes in the Tarim Basin. The research results of this paper show that, despite the warming and wetting trends since 1987 in the Tarim Basin, the climate type did not change. From 1987 to 2020, the main teleconnection factors of climate change in the Tarim Basin were PDO and ENSO.
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Tang, Congcang, Qiao Li, Hongfei Tao, Mahemujiang Aihemaiti, Zhenxia Mu, and Youwei Jiang. "Evaluation and driving factors of ecological environment quality in the Tarim River basin based on remote sensing ecological index." PeerJ 12 (October 28, 2024): e18368. http://dx.doi.org/10.7717/peerj.18368.

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Changes in the ecological environment quality (EEQ) in the main inland Tarim River Basin in China substantially impact the regional development. Indeed, comprehensive ecological environment measures have been implemented in the Tarim River Basin since 2000. In this context, the main objective of the present study was to investigate the spatiotemporal evolution of the EEQ and monitor the effectiveness of ecological restoration measures in the Tarim River Basin over the 2000–2020 period using remote sensing data. First, a Remote Sensing Ecological Index (RSEI) was constructed based on the Moderate Resolution Imaging Spectroradiometer remote sensing data. Second, the spatial distributions and factors of the RSEI were analyzed by using Moran’s Index and Geodetector. The results indicated that the overall RSEI values for the Tarim River Basin increased from 0.22 in 2000 to 0.25 in 2020. Moreover, the values for areas with poor EEQ decreased from 50.7% to 44.73%, while those with moderate EEQ increased from 11.45% to 16.91%. Therefore, the results demonstrated a slight overall improvement in the EEQ of the study area over the 2000–2020 period. On the other hand, the EEQ in the Tarim River Basin exhibited a significant spatial autocorrelation in the 2000–2020 period, with a relatively stable overall spatial distribution. Areas with high–high aggregation were distributed in the high-elevation mountainous areas in the western, northern, and southern parts of the study area. In contrast, areas with low–low aggregation were observed in the central and eastern low-elevation desert areas. The EEQ in the Tarim River Basin was driven by the interactions of several factors, including the normalized difference vegetation index, land surface moisture, land surface temperature, normalized differential build-up and bare soil index, and elevation. In particular, heat was the main driving factor that severely impacted the EEQ in the study area. Indeed, increase in the heat values could directly enhance meltwater runoff from glaciers in the basin, thereby resulting in short-term improvement in the basin EEQ. Furthermore, rapid urbanization from 2015 to 2020 resulted in a decrease in the average RSEI value of the Tarim River Basin by 0.1 over this period, consequently, the EEQ level decreased slightly. Briefly, the EEQ in the Tarim River Basin showed an overall increasing trend from 2000 to 2020, further demonstrating the effectiveness of a series of implemented ecological restoration measures in the Tarim River Basin over this period.
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Liu, Na, Kai-Yun, Guan, and Ying Feng. "Spatial Distribution Pattern ofCalligonumL. in Tarim Basin." Vegetos- An International Journal of Plant Research 27, no. 3 (2014): 58. http://dx.doi.org/10.5958/2229-4473.2014.00070.6.

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Jacob, Alexander. "The Riddle of the Tarim Basin Mummies." Mankind Quarterly 41, no. 4 (2001): 437–48. http://dx.doi.org/10.46469/mq.2001.41.4.4.

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Peng, Jue Yi, Zhan Ling Li, and Zhi Xia Xu. "Applicability Evaluation of WASMOD in Tarim Basin." Applied Mechanics and Materials 522-524 (February 2014): 902–6. http://dx.doi.org/10.4028/www.scientific.net/amm.522-524.902.

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Tarim basin,which located in north-west of China, is a very important zone both on ecology and economy. How much discharge could it produce has significant importance to the residents' life and the progress of this region. Beside of rainfall, the glaciers that existed plentifully in the upstreams have a great role in this basin which due to the very quantity of snow-melt. In this study, we choose Akesu river that belongs to this basin to be object. The WASMOD hydrologic model used in this program has both snow-melt and rainfall modules with eight sub-models. This article probed into different sub models applicabilities to Akesu river and came to a conclusion of which sub model was best suitable to it. On the basis of optimum model which calibrated by data from 1978-1987 monthly precipitation, evaporation, fast speed flow and base flow, we simulated real evaporation, slow flow, fast flow and total volume of runoff around 2001-2004.The result showed a good applicability of WASMOD in Tarim Basin.
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JIN, Zhijun. "Wave tectono-sedimentary processes in Tarim basin." Science in China Series D 48, no. 11 (2005): 1949. http://dx.doi.org/10.1360/04yd0087.

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Dissertations / Theses on the topic "Tarim Basin"

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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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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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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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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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Blayney, Tamsin. "Cenozoic evolution of the Pamir Salient : timing, mechanisms and paleo-environmental impacts : constraints from the Aertashi section, western Tarim Basin." Thesis, Lancaster University, 2017. http://eprints.lancs.ac.uk/88868/.

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The formation of the Himalayas and surrounding mountain ranges is one of the most significant tectonic events of the Cenozoic, with far reaching impacts on both regional and global climate. The Pamir represents the indented westward continuation of the northern margin of the Tibetan Plateau making them a key study area to examine internal deformation and intracontinental subduction processes. Yet the tectonics of the Pamir Salient is poorly understood. Much debate is ongoing, regarding the extent of indentation and mechanisms driving uplift of the Pamir. This project seeks to provide constraints on the timing of Pamir evolution and examine the impact of Pamir formation on the regional climate using a variety of techniques to date and interpret observed variations in terms of provenance, tectonism and climate, the results of which are presented here. At ~41 Ma the Tarim Sea retreated from the Aertashi region. Continental deposition ensued, dominated by the western Kunlun to the south. By 24-22 Ma, basinward expansion of the NW margin of Tibet coincides with the initiation of Pamir indentation. Activation of strike slip faulting, growth strata and exhumation along the Kashgar-Yecheng Transfer System is evidenced in the Aertashi region which may be linked to a pull-apart basin. By ~18.5 Ma, the onset of northward thrusting of the Kunlun hinterland and southward migrating foreland of the Tian Shan positions the Aertashi region in the depocenter of the Tarim Basin. By ~15 Ma, the Pamir Salient had propagated sufficiently far north, that the north Pamir, and by 11 Ma the Central Pamir were proximal to Aertashi. The Eocene – mid Miocene climate in the Tarim Basin was highly seasonal with evidence of increased aridity. Aridification was interrupted by a short period of increased humidity at ~17.6-15 Ma which can be linked to the mid-Miocene climate optimum, or a facies change. Limited comparative studies make climatic conclusions tentative.
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Yang, Yunyun. "Shifting Memories: Burial Practices and Cultural Interaction in Bronze Age China : A study of the Xiaohe-Gumugou cemeteries in the Tarim Basin." Thesis, Uppsala universitet, Institutionen för arkeologi och antik historia, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-386612.

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This study focuses on the burial practices in the Bronze Age Xiaohe-Gumugou cemeteries, north-west China, in order to understand how people constructed their social identities and delivered the social cognitions through generations. The Xiaohe-Gumugou cemeteries, as the main sites of the Xiaohe cultural horizon, have central roles for the understanding of the formation of the Bronze Age cultural groups and the cultural interactions between the west and the east in the Tarim Basin. However, current research is lacking in-depth examinations of the material culture of the cemeteries, and the contexts of the surrounding archaeological cultures in a timespan from Bronze Age to Iron Age. Through detailed comparisons of the construction of coffins and monuments, the dress of the dead, and the burial goods assemblages, this study provides an overview of the social structural development, from the Gumugou group’s heterogenous condition to the Xiaohe group’s homogeneous and mature state. Also, through relating to the results of biological and osteological analyses, and applying geographical analyses to the material, this study suggests that the early settlers in the Tarim Basin, the Xiaohe-Gumugou people have created their own social identities. Although the Xiaohe-Gumugou people might have migrated from southern Siberia or Central Asia, the archaeological material shows indications of their own typical features. When newcomers joined the society, the local burial customs were accepted and applied in a new cultural setting.<br>Denna studie fokuserar på gravskick på gravfälten Xiaohe och Gumugou i nordvästra Kina, för att förstå hur människor konstruerade social identitet och överförde kulturella föreställningar mellan generationer. Xiaohe-Gumugou-gravfälten, som de viktigaste platserna i Xiaohe-kulturhorisonten, är centrala för förståelsen av bildandet av bronsålderns kulturgrupper och de kulturella växelverkningarna mellan väst och öst i Tarimbäckenet. Tidigare forskning saknar fördjupade undersökningar av gravfältens materiella kultur samt den historiska kontexten med de omgivande arkeologiska kulturerna under tidsperioden från bronsålder till järnålder. Genom detaljerade jämförelser av konstruktionen av kistor och monument samt de dödas klädsel och gravgåvor, ger denna studie en översikt över utvecklingen av sociala strukturer, från Gumugou-gruppens heterogena situation till Xiaohe-gruppens homogena och mogna tillstånd. Genom att relatera till resultaten från biologiska och osteologiska analyser och tillämpa geografiska analyser på materialet, tyder den här studien på att de tidiga bosättarna i Tarimbäckenet, Xiaohe-Gumugou-folket, har utvecklat egna sociala identiteter. Trots att Xiaohe-Gumugou-folket kan ha migrerat från södra Sibirien eller Centralasien visar det arkeologiska materialet indikationer på egna typiska egenskaper. När nykomlingar anslöt till samhället accepterades de lokala begravningssederna och tillämpades i ett nytt kulturellt sammanhang.
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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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Wang, Anjia [Verfasser], and Roman [Akademischer Betreuer] Koch. "Combined Microfacies-Log-Analysis of Cambrian and Ordovician carbonate rocks (Upper Cambrian, Western Hills, Bejing; TZ-162 well, Tarim Basin, Western China) / Anjia Wang. Gutachter: Roman Koch." Erlangen : Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU), 2014. http://d-nb.info/1064996752/34.

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Books on the topic "Tarim Basin"

1

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

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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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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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Aijun, Qiu, and Zhang Ling 1977 October-, eds. Xinjiang Talimu Pendi ye sheng zhi wu ming lu: Native plants lists in Tarim Basin of Xinjiang. Ke xue chu ban she, 2013.

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Mingjiang, Deng, ed. Talimu He liu yu shui quan guan li yan jiu: On the management of water rights in Tarim river basin. Zhongguo shui li shui dian chu ban she, 2010.

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Yong, Hui. Gong gong wu pin guan li shi jiao xia de Talimu He liu yu shui tu zi yuan kai fa li yong: Water and soil resources development and utilization in the Tarim River Basin from the perspective of public management. Jing ji guan li chu ban she, 2012.

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

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From Sasanian Persia to the Tarim Basin: Pre-Islamic Iranian art and culture along the Silk-Road. WriteUp, 2021.

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Xinjiang Talimu Pendi ye sheng zhi wu tu pu: Native plants atlas in Tarim Basin of Xinjiang. Ke xue chu ban she, 2013.

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Book chapters on the topic "Tarim Basin"

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Kang, In Uk, Jinseong Han, Jong Ha Hong, Jieun Kim, Dong Hoon Shin, and Victor H. Mair. "Archaeological Findings of the Tarim Basin Graves and Mummies." In The Handbook of Mummy Studies. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-1614-6_28-1.

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Kang, In Uk, Jinseong Han, Jong Ha Hong, Jieun Kim, Dong Hoon Shin, and Victor H. Mair. "Archaeological Findings of the Tarim Basin Graves and Mummies." In The Handbook of Mummy Studies. Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-15-3354-9_28.

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Yang, Xiao-chuan, Li Li, Ning Yin, et al. "Fine Interpretation Method of Microstructure in a Oilfield, Tarim Basin." In Springer Series in Geomechanics and Geoengineering. Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-1964-2_158.

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Jiang, Na. "Characteristics of Silurian Sedimentary Reservoirs in Yingjisu Area, Tarim Basin." In Proceedings of the International Field Exploration and Development Conference 2021. Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-2149-0_492.

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Yingmin, Wang, Zhao Guanjun, Deng Lin, et al. "Assessment of Oil & gas Resources by 3-D Basin Modeling of Tarim Basin, China." In Geology of Fossil Fuels - Oil and Gas. CRC Press, 2021. http://dx.doi.org/10.1201/9780429087837-15.

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Li, Xin, Jin Jia, and Yue-dong Lu. "Geochemical and Geochronological Evidences of Neoproterozoic Tectonic Evolution in Tarim Basin." In Springer Series in Geomechanics and Geoengineering. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-97-0464-4_61.

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Ståhlberg, Sabira, and Ingvar Svanberg. "When Is a Foraging Society? The Loplik in the Tarim Basin." In Hunter-gatherers in a Changing World. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-42271-8_2.

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Hao, Qingqing, and Weijun Chen. "Petroleum exploration potential of the Yaken uplift in northern Tarim Basin." In Advances in Geology and Resources Exploration. CRC Press, 2022. http://dx.doi.org/10.1201/9781003308584-65.

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Keming, Yang, Chen Zhaoguo, Gong Ming, and Wu Yajun. "Deformational Characteristics and Oil/Gas Accumulation in Tarim Basin of China." In Geology of Fossil Fuels - Oil and Gas. CRC Press, 2021. http://dx.doi.org/10.1201/9780429087837-25.

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Du, Zhong-yuan, Xiang-wen Li, Qing-lin Li, Zi-ao Wang, and Chun-yang Wang. "Fracture Modeling and Connectivity Analysis in Northern Yueman, Fuman Oilfield, Tarim Basin." In Springer Series in Geomechanics and Geoengineering. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-97-0468-2_38.

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Conference papers on the topic "Tarim Basin"

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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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Jun, Tian, Peng Gengxin, Chen Meng, et al. "Application of joint tomography to Tarim Basin Foothill imaging." In SEG Technical Program Expanded Abstracts 2018. Society of Exploration Geophysicists, 2018. http://dx.doi.org/10.1190/segam2018-2997996.1.

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Bandyopadhyay, Debmita, Gulab Singh, Girjesh Dasaundhi, Nela Bala Raju, Akshay Patil, and Shradha Mohanty. "Surging Glacier Dynamics in Tarim Basin Using SAR Data." In IGARSS 2020 - 2020 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2020. http://dx.doi.org/10.1109/igarss39084.2020.9323095.

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Wang, Guizhong, Zhiyong Wang, and Yongxing Gu. "Tarim basin Kuqa depression piedmont complex structural interpretation technology." In Beijing 2009 International Geophysical Conference and Exposition. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3603672.

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Feng, Y., H. L. Xin, Y. Li, and W. J. Li. "Spatial Distribution Pattern of Nitraria L. in Tarim Basin." In International Workshop on Environmental Management, Science and Engineering. SCITEPRESS - Science and Technology Publications, 2018. http://dx.doi.org/10.5220/0007560002850290.

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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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Duan, Wensheng, Genxin Peng, Xiaoping Song, and Xueqiang Li. "Local angle domain imaging and fracture predction in Tarim Basin." In SEG Technical Program Expanded Abstracts 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/segam2017-17677545.1.

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Di, G. D., S. Z. Sun, X. Q. Pang, L. F. Liu, and L. Chen. "Comprehensive Prediction for Fractured Carbonate Reservoir in the Tarim Basin." In 77th EAGE Conference and Exhibition 2015. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413399.

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Ma, Zhixia, Sam Zandong Sun, Haijun Bai, and Wenbo Sun. "3C–3D VSPPPandPSVimaging in the Lungu 38 area, Tarim Basin." In SEG Technical Program Expanded Abstracts 2009. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3255739.

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