Journal articles: 'Tarim Basin'

1

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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2

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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4

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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5

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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7

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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8

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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9

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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10

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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11

Longde, Sun, Jiang Tongwen, Xu Hanlin, Shan Jiazeng, and Lian Zhanggui. "Unsteady reservoir in Hadson Oilfield, Tarim Basin." Petroleum Exploration and Development 36, no. 1 (2009): 62–67. http://dx.doi.org/10.1016/s1876-3804(09)60111-7.

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12

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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13

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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14

Junmeng, Zhao. "Clockwise rotation of the Tarim basin driven by the Indian plate impact. Part II*." Earth sciences and subsoil use 43, no. 4 (2021): 486–98. http://dx.doi.org/10.21285/2686-9993-2020-43-4-486-498.

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In the previous article**, data were given on the clockwise rotation of the Tarim Basin at a speed of 0.461° per million years around a virtual axis within the structure. Additional fieldwork and new evidence confirm earlier findings about the asymmetry of the Indo-Asian collision zone. These data are additional arguments in favor of the rotation of the Tarim Basin and lithospheric interactions along the Tarim boundaries. Conclusions are based on detailed geological and geophysical data.

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15

Cheng, Lei, Dan Song, Xiaoli Yu, Xue Du, and Tangbin Huo. "Endangered Schizothoracin Fish in the Tarim River Basin Are Threatened by Introgressive Hybridization." Biology 11, no. 7 (2022): 981. http://dx.doi.org/10.3390/biology11070981.

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Big-head Schizothoracin (Aspiorhynchus laticeps) and Tarim Schizothoracin (Schizothorax biddulphi) are locally sympatric in the Tarim River Basin. Although another Schizothoracin (Schizothorax esocinus) in Tarim River basin has been speculated to be hybrid offspring of Big-head Schizothoracin and Tarim Schizothoracin, there was no genetic evidence. Previous studies on the genetics and evolution of Schizothoracins in Xinjiang Province were mostly based on mitochondrial DNA (mtDNA), whose characteristics of maternal inheritance made it hard to answer the question of whether there was hybridization and introgression between Big-head Schizothoracin and Tarim Schizothoracin. In this study, cytochrome b (cytb) gene of mtDNA and internal transcribed spacer 2 (ITS2) that is encoded by the nuclear genome were genotyped within the entire samples at the same time. Our results confirmed that Schizothorax esocinus was the hybrid offspring of Big-head Schizothoracin and Tarim Schizothoracin. The heterozygous ITS2 genotypes and/or Aspiorhynchus laticeps-like mtDNA were also detected in a subset of samples that should have been identified as pure Schizothorax biddulphi based on morphology. The ITS2 is characterized by multi-copy, concert evolution, and biparental inheritance. Thus, by comparing with mtDNA data, broad-scale bidirectional hybridization and introgression between Big-head Schizothoracin and Tarim Schizothoracin were revealed. Although interspecific hybridization may play a positive role in ecology and evolution, interspecific hybrids could threaten their parental species by the swamping of genetics and demography. As both parents of hybridization are critically endangered fishes, in this case, it is urgently necessary to strengthen the scientific assessment of the risks of the hybrids and the control of the hybridization and introgression between Aspiorhynchus laticeps and Schizothorax biddulphi in the Tarim River Basin.

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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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Lu, Quan, Fengjiao Liu, Yanjun Li, and Dezhen Wang. "Study on the Relationship between Water Resources Utilization and Economic Growth in Tarim River basin from the Perspective of Water Footprint." Water 14, no. 10 (2022): 1655. http://dx.doi.org/10.3390/w14101655.

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Taking the Tarim River basin as the research object, the water footprint was calculated based on the water footprint theory based on the relevant data from 2008 to 2019, and the water resource evaluation system was constructed to analyze the water footprint and water resource utilization of the Tarim River basin from three levels of structure, benefit, and ecology. Based on the water footprint theory, the annual water footprint and GDP of Tarim River basin were used to construct the Tapio decoupling model, and the decoupling type between water resources utilization and economic growth was obtained. The relationship between water resource utilization and economic growth in Tarim River was analyzed by combining the decoupling type evaluation and water footprint evaluation. The internal benefit is poor, and the external benefit is good; The degree of water resource shortage is on the rise, and the self-sufficiency rate of water resources is large. On the whole, the decoupling strength increases gradually. Decoupling strength has obvious industrial influence characteristics. Based on the above research conclusions, the sustainable economic and ecological development of the Tarim River basin can be realized from two aspects: reducing water footprint and strengthening decoupling intensity.

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Zhang, Fan, Chao Ning, Ashley Scott, et al. "The genomic origins of the Bronze Age Tarim Basin mummies." Nature 599, no. 7884 (2021): 256–61. http://dx.doi.org/10.1038/s41586-021-04052-7.

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AbstractThe identity of the earliest inhabitants of Xinjiang, in the heart of Inner Asia, and the languages that they spoke have long been debated and remain contentious1. Here we present genomic data from 5 individuals dating to around 3000–2800 bc from the Dzungarian Basin and 13 individuals dating to around 2100–1700 bc from the Tarim Basin, representing the earliest yet discovered human remains from North and South Xinjiang, respectively. We find that the Early Bronze Age Dzungarian individuals exhibit a predominantly Afanasievo ancestry with an additional local contribution, and the Early–Middle Bronze Age Tarim individuals contain only a local ancestry. The Tarim individuals from the site of Xiaohe further exhibit strong evidence of milk proteins in their dental calculus, indicating a reliance on dairy pastoralism at the site since its founding. Our results do not support previous hypotheses for the origin of the Tarim mummies, who were argued to be Proto-Tocharian-speaking pastoralists descended from the Afanasievo1,2 or to have originated among the Bactria–Margiana Archaeological Complex3 or Inner Asian Mountain Corridor cultures4. Instead, although Tocharian may have been plausibly introduced to the Dzungarian Basin by Afanasievo migrants during the Early Bronze Age, we find that the earliest Tarim Basin cultures appear to have arisen from a genetically isolated local population that adopted neighbouring pastoralist and agriculturalist practices, which allowed them to settle and thrive along the shifting riverine oases of the Taklamakan Desert.

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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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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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Pan, Yun, Zong Xiu Wang, and Mao Pan. "Redefined Distribution of the Permian Volcanic Rocks in the Tarim Basin: Based on Logging and Seismic Data." Applied Mechanics and Materials 448-453 (October 2013): 3723–27. http://dx.doi.org/10.4028/www.scientific.net/amm.448-453.3723.

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There are a lot of Permian volcanic rocks which are widely distributed in Tarim Basin. Because of the shielding effect of the volcanic rocks to the underlying structure, the distribution of the volcanic rocks in Tarim Basin is very important to the deep oil and gas exploration. However, with the progress of oil exploration in Tarim oil field in recent years, much more logging and seismic data is available. Based on the model of logging-seismic integrated identification, the distribution of the Permian volcanic rocks is revised by using the drilling, logging and seismic data. It shows that the rhyolite is mainly distributed in the north basin, and the basalt is widely distributed in the basin. Moreover, the basalt has larger area than which delineated by other people.

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Wang, Qian, Sanzhong Li, Shujuan Zhao, Dunling Mu, Runhua Guo, and Ian Somerville. "Early Paleozoic Tarim Orocline: Insights from paleogeography and tectonic evolution in the Tarim Basin." Geological Journal 52 (August 31, 2017): 436–48. http://dx.doi.org/10.1002/gj.2985.

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LYUBOV V., GLEBOVA, CHI QINGYUAN, and SEREBRYAKOV ANDREY O. "REGIONAL GEOLOGICAL STUDIES OF DOME-SHAPED UPLIFTS OF THE TARIM SEDIMENTARY BASIN." Geology, Geography and Global Energy 81, no. 2 (2021): 31–41. http://dx.doi.org/10.21672/2077-6322-2021-81-2-031-041.

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He regional geological study of the Tarim sedimentary basin, located in the tectonic zone of the Donkhetang fault, is of national interest. The Tarim sedimentary basin is an ultradeep and complex basin. A number of anticline structures are confined to the central part of the Tabei uplift. In the structure of the tectonic belt, two inversion faults take part, with the formation of a structural nose. Domed uplifts lie at a depth of 6000 meters, the thickness of the prospective layers reaches 20 meters. Combining regional geological studies and the results of sedimentary facies studies, the rocks of the prospective formations are a transgressively controlled sandstone layer, which uses the environment of deltaic sediments as a background. Based on the results of modern sedimentary studies, the characteristics of the Donghae sandstone are analyzed. To study the Tarim sedimentary basin, a complex of regional studies related to the geological study, the tectonic structure of the region, lithological-stratigraphic studies, sequence-stratigraphic studies, studies of the physical and reservoir properties of rocks, regional studies of the thickness, uniformity and strike of the studied layers was carried out. The main target objects are a group of reservoirs of the Jurassic and Carboniferous periods. Proven geological reserves of oil and gas have been recorded in the Tarim sedimentary basin.

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Zhang, Qinqin, Fang Gu, Sicong Zhang, Xuehua Chen, Xue Ding, and Zhonglin Xu. "Spatiotemporal Variation in Wind Erosion in Tarim River Basin from 2010 to 2018." Land 13, no. 3 (2024): 330. http://dx.doi.org/10.3390/land13030330.

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The Tarim River Basin, China’s largest inland river basin, is renowned for its ecological fragility characterized by concurrent greening and desertification processes. Soil wind erosion emerges as a critical factor impacting the natural ecosystem of this region. This study employs a soil wind erosion model tailored to cultivated land, grassland, and desert terrains to analyze the multitemporal characteristics of and spatial variations in soil wind erosion across nine subbasins within the Tarim River Basin, utilizing observed data from 2010, 2015, and 2018. Additionally, this study investigates the influence of various factors, particularly wind speed, on the soil wind erosion dynamics. Following established standards of soil erosion classification, the intensity levels of soil erosion are assessed for each calculation grid within the study area alongside an analysis of the environmental factors influencing soil erosion. Findings indicate that approximately 38.79% of the total study area experiences soil wind erosion, with the Qarqan River Basin exhibiting the highest erosion modulus and the Aksu River Basin registering the lowest. Light and moderate erosion predominates in the Tarim River Basin, with an overall decreasing trend observed over the study period. Notably, the Qiemo River Basin, Dina River Basin, and Kaidu Kongque River Basin display relatively higher proportions of eroded area compared to their total subbasin area. Furthermore, this study underscores the substantial influence of the annual average wind speed on soil erosion within the study area, advocating for prioritizing soil and water conservation programs, particularly in the downstream regions of the Tarim River Basin, to mitigate future environmental degradation.

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Guo, Jian, and Diandong Zhao. "Seismic exploration in desert area of Tarim basin." ASEG Extended Abstracts 2010, no. 1 (2010): 1–3. http://dx.doi.org/10.1081/22020586.2010.12041903.

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Xiaoan, Xie, Li Guangwen, and Huang Yaping. "China’s Tarim Basin poses singular seismic surveying problems." Leading Edge 15, no. 4 (1996): 293. http://dx.doi.org/10.1190/1.1437322.

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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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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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29

Tang, Qicheng, and Hongyan Chen. "Water resources and oasis construction in Tarim Basin." Chinese Geographical Science 2, no. 2 (1992): 173–82. http://dx.doi.org/10.1007/bf02664539.

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Zhao, JunMeng, HongGang Cheng, ShunPing Pei, HongBing Liu, JianShi Zhang, and BaoFeng Liu. "Deep structure at northern margin of Tarim Basin." Science Bulletin 53, no. 10 (2008): 1544–54. http://dx.doi.org/10.1007/s11434-008-0117-8.

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Jia, Chengzao, and Guoqi Wei. "Structural characteristics and petroliferous features of Tarim Basin." Chinese Science Bulletin 47, S1 (2002): 1–11. http://dx.doi.org/10.1007/bf02902812.

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32

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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Hou, Bing, Shui Xiang Xie, Mian Chen, Guan Cheng Jiang, Yan Jin, and Chuan Liang. "New Method of Layered Drilling Fluid Design to Overcome Wellbore Instability of Piedmont Structures." Advanced Materials Research 524-527 (May 2012): 1480–83. http://dx.doi.org/10.4028/www.scientific.net/amr.524-527.1480.

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This paper will take the complex layer of the Qunkuqiake region of Tarim Basin as a research object in order to find the reasons of the borehole instability. The layered drilling fluid design technique is put forward firstly and a new drilling fluid technology to solve the problems of wall instability of the Qunkuqiake regions in Tarim Basin is developed.

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Lu, Quan, Yanxia Yang, Bo Li, Yanjun Li, and Dezhen Wang. "Coupling Relationship and Influencing Factors of the Water–Energy–Cotton System in Tarim River Basin." Agronomy 12, no. 10 (2022): 2333. http://dx.doi.org/10.3390/agronomy12102333.

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As the largest inland river basin in China, the Tarim River Basin is an important energy base and a key cotton-producing area in China. Therefore, the harmonious development of water resources, energy resources and cotton resources in the Tarim River Basin is a lifeline for stable quality and efficient development in this region. In this paper, the water–energy–cotton system of the Tarim River Basin is constructed and the weight of each index in the system is determined by using the entropy method. On this basis, the comprehensive development index of each subsystem and the water–energy–cotton system is calculated to measure the comprehensive development level of each system. Then, the coupling relationship between the three resources is quantitatively analyzed by using the coupling coordination degree model, and the mutual influence and strength of interaction between each system are calculated. Finally, a fractional regression model is established to analyze the factors affecting the coordinated development of the water–energy–cotton system in the Tarim River Basin. The results show that the comprehensive development index of the Tarim River Basin fluctuates obviously and the comprehensive development level of water resource systems is higher than that of the cotton resource and energy resource systems, and there are regional differences between each subsystem and the comprehensive development index of water–energy–cotton system. The coupling coordination degree of the basin is the primary coordination on the whole; however, there are significant differences in the coupling coordination degree of each region. In terms of influencing factors, the area of soil erosion treatment and water consumption in ecological environments both play a positive role in promoting the coupling coordination degree, and population size and GDP will hinder the development of the coupling coordination degree to a certain extent.

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Sun, Weicheng, and Xingfu Zhang. "Revealing Water Storage Changes and Ecological Water Conveyance Benefits in the Tarim River Basin over the Past 20 Years Based on GRACE/GRACE-FO." Remote Sensing 16, no. 23 (2024): 4355. http://dx.doi.org/10.3390/rs16234355.

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As China’s largest inland river basin and one of the world’s most arid regions, the Tarim River Basin is home to an extremely fragile ecological environment. Therefore, monitoring the water storage changes is critical for enhancing water resources management and improving hydrological policies to ensure sustainable development. This study reveals the spatiotemporal changes of water storage and its driving factors in the Tarim River Basin from 2002 to 2022, utilizing data from GRACE, GRACE-FO (GFO), GLDAS, the glacier model, and measured hydrological data. In addition, we validate GRACE/GFO data as a novel resource that can monitor the ecological water conveyance (EWC) benefits effectively in the lower reaches of the basin. The results reveal that (1) the northern Tarim River Basin has experienced a significant decline in terrestrial water storage (TWS), with an overall deficit that appears to have accelerated in recent years. From April 2002 to December 2009, the groundwater storage (GWS) anomaly accounted for 87.5% of the TWS anomaly, while from January 2010 to January 2020, the ice water storage (IWS) anomaly contributed 57.1% to the TWS anomaly. (2) The TWS changes in the Tarim River Basin are primarily attributed to the changes of GWS and IWS, and they have the highest correlation with precipitation and evapotranspiration, with grey relation analysis (GRA) coefficients of 0.74 and 0.68, respectively, while the human factors mainly affect GWS, with an average GRA coefficient of 0.64. (3) In assessing ecological water conveyance (EWC) benefits, the GRACE/GFO-derived TWS anomaly in the lower reaches of the Tarim River exhibits a good correspondence with the changes of EWC, NDVI, and groundwater levels.

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Sobel, Edward R. "Basin analysis of the Jurassic–Lower Cretaceous southwest Tarim basin, northwest China." Geological Society of America Bulletin 111, no. 5 (1999): 709–24. http://dx.doi.org/10.1130/0016-7606(1999)111<0709:baotjl>2.3.co;2.

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Wei, Guoqi, Chengzao Jia, Benliang Li, and Hanlin Chen. "Silurian to Devonian foreland basin in the south edge of Tarim Basin." Chinese Science Bulletin 47, S1 (2002): 42–46. http://dx.doi.org/10.1007/bf02902817.

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Guo, Junhao, Xinbao Lian, and Xueqiu Wang. "Electrical Conductivity Evidence for the Existence of a Mantle Plume Beneath Tarim Basin." Applied Sciences 11, no. 3 (2021): 893. http://dx.doi.org/10.3390/app11030893.

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This paper proposes using a simulated annealing (SA) calculation to perform one-dimensional inversion of Geomagnetic Depth Sounding (GDS) to obtain the conductivity information of the lower mantle beneath the Tarim area, to calculate the temperature of the lower mantle according to the relevant formula of the petrophysical experiment, and to provide evidence of the existence of the Tarim mantle plume. The data used for inversion originate from the China Geomagnetic Network Center. This article uses theoretical data to prove that the simulated annealing algorithm can invert the true conductivity model when the data do not contain noise. However, when the data contain noise, it is more accurate to use the statistical expected value of the high-quality conductivity model during the simulated annealing inversion process as the optimal conductivity model rather than the classic simulated annealing algorithm. The simulated annealing inversion results of only four stations in Tarim area show that the conductivity of the top of the lower mantle and the upper part of the mantle transition zone in Tarim area is higher than the global average, and it is speculated that the temperature is 150k–450k higher than the global average. This is important evidence for the existence of the mantle plume beneath the Tarim Basin.

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Wang, Yichu, Danlu Liu, Enhang Liang, and Jinren Ni. "Structural Characteristics of Endorheic Rivers in the Tarim Basin." Remote Sensing 14, no. 18 (2022): 4502. http://dx.doi.org/10.3390/rs14184502.

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Endorheic rivers as landlocked systems with no hydrological connections to marine environments are suffering from water and ecosystem crisis worldwide, yet little is known about their structural characteristics with complex geomorphic and climatic dependence. Based on the river networks identified from 30 m resolution digital elevation models and surface water dynamic information derived from Landsat images, we investigate the hierarchical characteristics of 60 sub-basins in the Tarim Basin, the largest endorheic river basin in China. In the Tarim River basin, endorheic rivers exhibit a self-similarity only in the range of stream-orders 1–4, compared to the range of stream-orders 1–5 observed in exorheic rivers, owning to the limited stream power to maintain the similar aggregation of rivers in the arid regions. Moreover, the Tarim River networks demonstrate lower bifurcation ratio (2.48), length ratio (2.03), fractal dimension (1.38), and drainage density (0.24 km−1) in representative sub-basins, with a significant decay in median values compared with those derived from exohreic rivers at similar scales, suggesting sparser and imperfect developed branching river networks in endorheic basins. Further analysis on the Tarim reveals that endorheic river structure is more related to glacier extent (r = 0.67~0.84), potential evapotranspiration (r = 0.63~0.81), and groundwater type index (r = 0.64~0.73), which is essentially different from the structure of exorheic river represented by the Yellow River largely controlled by surface runoff, precipitation, and vegetation coverage. This study stresses the differences in intrinsic structural characteristics and extrinsic drivers of endorheic and exorheic rivers and highlights the necessity of differentiated strategies for endorheic river management in fragile ecosystems.

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Zhijun, Jin, Liu Quanyou, Qiu Nansheng, Ding Feng, and Bai Guoping. "Phase States of Hydrocarbons in Chinese Marine Carbonate Strata and Controlling Factors for Their Formation." Energy Exploration & Exploitation 30, no. 5 (2012): 753–73. http://dx.doi.org/10.1260/0144-5987.30.5.753.

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Chinese marine strata were mainly deposited before the Mesozoic. In the Tarim, Sichuan and Ordos Basins, the marine source rocks are made of sapropelic dark shale, and calcareous shale, and they contain type II kerogen. Because of different burial and geothermal histories, the three basins exhibit different hydrocarbon generation histories and preservation status. In the Tarim Basin, both oil and gas exist, but the Sichuan and Ordos Basins host mainly gas. The Tarim Basin experienced a high heat flow history in the Early Paleozoic. For instance, heat flow in the Late Cambrian varied between 65–75 mW/m2, but it declined thereafter and averages 43.5mW/m2 in the current time. Thus, the basin is a “warm to cold basin”. The Sichuan Basin experienced an increasing heat flow through the Early Paleozoic to Early Permian, and peaked in the latest Early Permian with heat flows of 71–77 mW/m2. Then, the heat flow declined stepwise to the current value of 53.2 mW/m2. Thus, it is a generally a high heat flow “warm basin”. The Ordos Basin has a low heat flow for most of its history (45–55 mW/m2), but experienced a heating event in the Cretaceous, with the heat flow rising to 70–80 mW/m2. Thus, this basin is a “cold to warm basin”. The Tarim Basin experienced three events of hydrocarbon accumulations. Oil accumulation formed in the late stage of Caledonian Orogeny. The generation and accumulation of oil continued in the Northern and Central Tarim (Tabei and Tazhong) till the late Hercynian Orogeny, during which, the accumulated oil cracked into gas in the Hetianhe area and Eastern Tarim (Tadong). In the Himalaya Orogeny, oil cracking occurred in the entire basin, part of the oil in the Tabei and Tazhong areas and most of the oil in the Hetianhe and Tadong areas are converted into gas. In the Sichuan Basin, another triple-episode generation and accumulation history is exhibited. In the Indosinian Orogeny, oil accumulation formed, but in the Yanshanian Orogeny, part of the oil in the eastern Sichuan Basin and most of the oil in the northeastern part was cracked into gas. In the Himalayan Orogeny, oil in the entire basin was converted into gas. The Ordos Basin experienced a double-episode generation and accumulation history, oil accumulation happened in the early Yanshanian stage, and cracked in the late stage. In general, multiple phases of heat flow history and tectonic reworking caused multiple episodes of hydrocarbon generation, oil to gas cracking, and accumulation and reworking. The phases and compositions of oil and gas are mainly controlled by thermal and burial histories, and hardly influenced by kerogen types and source rock types.

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WANG, Peng, Xiangyi LI, Repkat Repkat, Lisha LIN, and Fanjiang ZENG. "A dataset of monthly litter recovery from the desert grassland in Southern Tarim Basin during 2010–2020." China Scientific Data 9, no. 2 (2024): 1–5. http://dx.doi.org/10.11922/11-6035.csd.2023.0146.zh.

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The Cele National Field Science Observation and Research Station of Desert Grassland Ecosystem of Xinjiang of Chinese Academy of Science (Hereinafter referred to as "Cele Station"), is located on the southern margin of the Tarim Basin bordered to the south by the Kunlun Mountains and to the north by the largest desert in China, the Taklimakan Desert. As a result of simple vegetation community and slow accumulation of soil organic matter, litter serves as an important source of nutrients in this area. Based on the long-term observations of desert plant communities at Cele station, we gathered monthly dynamic data of litter recovery in the desert grassland from Southern Tarim Basin from 2010 to 2020. Based on plant organs (branches, leaves, and fruits), the monthly dynamic data of litter recovery at the observation sites and plots were sorted out, and the annual changes of community and soil nutrients were recorded. Data were compiled in strict accordance with CERN bio-observation specifications. The data has undergone review and quality control by the quality control personnel of the station and sub-center. The results would provide basic data for further study of litter dynamics in the desert grassland from Southern Tarim Basin, and theoretical support for better understanding and assessing nutrient cycling in hyper–arid desert ecosystems.

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Zhu, Feng. "Distribution Regularity of the Ordovician Reef-Bank Reservoir inside Sequence Stratigraphic Framework in Central Tarim Basin." Applied Mechanics and Materials 484-485 (January 2014): 612–15. http://dx.doi.org/10.4028/www.scientific.net/amm.484-485.612.

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Based on the integrated study of the outcrops, the seismic, drilling and logging data of Lianglitage formation in central Tarim Basin, the sequence stratigraphic framework of the platform margin is built, and the Lianglitage formation is divided into 3 third-order sequences. The vertical pattern and lateral distribution for carbonate reef-bank reservoir in sequence stratigraphic framework are analyzed. The reef-bank reservoir mainly developed in highstand system tract of sequence Ssq2, and distributed along the carbonate platform margin of the Middle-Late Ordovician in central Tarim Basin. The mudstone mound, organic reef, granule bank are vertically stacked. Laterally, the area of well shun3-shun4-shun2-shun6 are characterized by multiphase bank reservoir overlapping, and the area of well TZ82-TZ44 - TZ161-TZ24 - TZ26 are characterized by multiphase organic reef and bank overlapping. The reef-bank complexes in sequence Ssq2 are the main targets of exploration in central Tarim Basin.

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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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Meng, Lihong, Youcun Liu, Weijing Ma, Qingyun Wang, Xiaoli Mo, and Jinming Tian. "Variable fuzzy evaluation model for water resources carrying capacity in the Tarim River Basin, China." Water Supply 22, no. 2 (2021): 1445–58. http://dx.doi.org/10.2166/ws.2021.341.

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Abstract As one of the regions of China with the most serious water-shortages, the shortage of water resources and ecological deterioration of the Tarim River Basin have increasingly attracted attention, and management and sustainable utilization of water resources rely mostly on the understanding of their carrying capacity. In the present study, the water resources carrying capacity of the Tarim River Basin was evaluated using a multi-dimensional perspective of natural, social and economic factors based on a variable fuzzy evaluation model for the 2018 hydroclimatic conditions. Evaluation model results rated Aksu, Kizilsu, Kashi and Hotan districts as grade 2, where current use and overexploitation of water resources have reached a relatively high level combined with a limited water resources carrying capacity. Bazhou district, where the water resources carrying capacity is relatively higher, was evaluated and rated as grade 1 by the model. It is urgent to put forward some strategies in order to protect and improve the water resources carrying capacity in the Tarim River Basin, which include promoting more efficient utilization of water conservation schemes, strengthening the long-term investment in environmental protection, improving the ratio of industrial wastewater treatment and reducing the industrial water quota. The results of the present study are aimed to be a beneficial guide in the planning and management of the Tarim River Basin water resources and possibly for other similar river basins.

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Zhang, Hongquan, and Zhuguo Ma. "Stability and tilting of regional water cycle over Tarim Basin." Proceedings of the International Association of Hydrological Sciences 379 (June 5, 2018): 31–36. http://dx.doi.org/10.5194/piahs-379-31-2018.

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Abstract. The Tarim Basin is located upwind of the Gobi Desert where individual deserts have expanded significantly during the last 50 years. In recent history, stable runoff in the Tarim Basin has been observed despite the Lop Nur dry up and dramatic water consumption shift from east to west. This regional water cycle stability is conceptually explained based on the relationship between precipitation and evapotranspiration. The water consumption imbalance is caused by human activities near the river sources, which tilts the humidity profile over the basin. As a result, more water vapour spills from the western part of the basin and causes precipitation to increase in adjacent areas. At the same time, the Westerlies carry the low humidity air mass out of the eastern part of the basin to make the downwind Gobi Desert and surrounding areas drier. Therefore, the observed wetting on the west and drying on the east of northwest China are coupled.

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Wu, Yunlong, Feng Liang, Jianguo Yan, Junling Pei, and Yi Zhang. "Analysis of Regional and Residual Gravity Disturbance of Major Fault Belts in the Tarim Basin, Western China." Remote Sensing 14, no. 16 (2022): 3948. http://dx.doi.org/10.3390/rs14163948.

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Large fault belts often influence the paleo-geomorphic changes in basins and control hydrocarbon accumulation and distribution in basins. Based on the gravity field model European Improved Gravity model of the Earth via New techniques (EIGEN)-6C4, this study calculated the residual Bouguer gravity disturbance of the Tarim Basin by using the minimum curvature method and analyzed gravitational characteristics of major fault belts of the Tarim Basin. The residual Bouguer disturbance exhibits linear residual Bouguer disturbance zones in the Tianshan Mountains, West Kunlun, and the Altyn region, which is consistent with the spatial distribution of their related fault belts. The regional Bouguer disturbance is related to crust–mantle boundary depth, which can be used to roughly estimate crust thickness. Thus, we suggest that the crust–mantle boundary depth order of major faults from deep to shallow is the Altyn region, West Kunlun, and Tianshan Mountains. There is a discontinuity in the residual Bouguer disturbance of West Kunlun, which compares well with the fault belt of West Kunlun. Furthermore, the residual Bouguer disturbance of the Tarim Basin has a series of elliptical areas with a central positive disturbance located within the Bachu uplift and other uplift structures. The residual Bouguer disturbance also reflects the position and distribution of the major fault belts and the boundary of the Tarim Basin, which can provide guidance for dynamic evolution analysis of large basins.

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Sabirhazi, Gulnur, XiaoShan Kang, Maryamgul Abdurahman, Ying Feng, XiYong Wang, and BoRong Pan. "Morphological Variation inCalligonum roborowskii(Polygonaceae) in the Tarim Basin." Vegetos- An International Journal of Plant Research 27, no. 3 (2014): 179. http://dx.doi.org/10.5958/2229-4473.2014.00086.x.

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Gulnur Sabirhazi, 古丽努尔·沙比尔哈孜, 潘伯荣 PAN Borong, and 段士民 DAUN Shimin. "The community characteristics ofCalligonum roborowskiiA. Los in Tarim Basin." Acta Ecologica Sinica 32, no. 10 (2012): 3288–95. http://dx.doi.org/10.5846/stxb201104120477.

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Zheng, Zehao, Brenton Sharratt, Gary Feng, Xinhu Li, and Huawei Pi. "Wind Erosion of Cropland in the Northwestern Tarim Basin." Soil Science Society of America Journal 80, no. 3 (2016): 672–82. http://dx.doi.org/10.2136/sssaj2015.07.0259.

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Andreev, Plamen S., Wenjin Zhao, Nian-Zhong Wang, et al. "Early Silurian chondrichthyans from the Tarim Basin (Xinjiang, China)." PLOS ONE 15, no. 2 (2020): e0228589. http://dx.doi.org/10.1371/journal.pone.0228589.

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Journal articles on the topic 'Tarim Basin'

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