Journal articles: 'Tarim Basin'

1

Norin, Erik. "Tertiary of the Tarim Basin*." Bulletin of the Geological Society of China 14, no. 3 (May 29, 2009): 337–48. http://dx.doi.org/10.1111/j.1755-6724.1935.mp14003006.x.

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2

Hai, H. E., and L. U. Guihua. "Precipitation Recycling in Tarim River Basin." Journal of Hydrologic Engineering 18, no. 11 (November 2013): 1549–56. http://dx.doi.org/10.1061/(asce)he.1943-5584.0000503.

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3

Chen, Hanlin, Shufeng Yang, Chuanwan Dong, Guoqiang Zhu, Chengzao Jia, Guoqi Wei, and Zhengguo Wang. "Geological thermal events in Tarim Basin." Chinese Science Bulletin 42, no. 7 (April 1997): 580–84. http://dx.doi.org/10.1007/bf03182623.

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4

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 (October 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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5

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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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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7

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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8

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 (February 2009): 62–67. http://dx.doi.org/10.1016/s1876-3804(09)60111-7.

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9

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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10

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 (September 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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11

Chang, Hong, Zhisheng An, Weiguo Liu, Hong Ao, Xiaoke Qiang, Yougui Song, and Zhongping Lai. "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 (May 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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12

Junmeng, Zhao. "Clockwise rotation of the Tarim basin driven by the Indian plate impact. Part II*." Earth sciences and subsoil use 43, no. 4 (January 28, 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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13

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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14

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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15

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 (January 2000): 1–12. http://dx.doi.org/10.1016/s0264-8172(99)00050-1.

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16

Huafu, Lu, David G. Howell, Jia Dong, Cai Dongsheng, Wu Shimin, Chen Chuming, Shi Yangshen, Zenon C. Valin, and Guo Lirh. "Kalpin Transpression Tectonics, Northwestern Tarim Basin, Western China." International Geology Review 36, no. 10 (October 1994): 975–81. http://dx.doi.org/10.1080/00206819409465499.

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17

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

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18

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

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19

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

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20

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

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21

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

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22

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 (May 2008): 1544–54. http://dx.doi.org/10.1007/s11434-008-0117-8.

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23

Zhao, Yong, Anning Huang, Yang Zhou, Danqing Huang, Qing Yang, Yufen Ma, Man Li, and Gang Wei. "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 (June 5, 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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24

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 (January 20, 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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25

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 (December 2002): 42–46. http://dx.doi.org/10.1007/bf02902817.

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26

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

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27

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 (September 11, 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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28

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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29

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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30

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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31

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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32

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 (May 2016): 672–82. http://dx.doi.org/10.2136/sssaj2015.07.0259.

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33

Tang, Zihua. "Placing prehistorical civilizations of Tarim Basin into climatic contexts." Quaternary International 279-280 (November 2012): 484. http://dx.doi.org/10.1016/j.quaint.2012.08.1638.

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34

Wang, Run, and Qianzhao Gao. "Preliminary study on flash floods in Tarim River basin." Chinese Geographical Science 7, no. 1 (March 1997): 53–58. http://dx.doi.org/10.1007/s11769-997-0072-3.

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35

ZHAO, Meng-jun, Zhao-ming WANG, Wen-qing PAN, Shao-bo LIU, Sheng-fei QIN, and Jian-fa HAN. "Lower Palaeozoic source rocks in Manjiaer Sag, Tarim Basin." Petroleum Exploration and Development 35, no. 4 (August 2008): 417–23. http://dx.doi.org/10.1016/s1876-3804(08)60089-0.

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36

Xiangbin, YAN, LI Tiejun, and ZHANG Tao. "Ordovician Basement Hydrocarbon Reservoirs in the Tarim Basin, China." Acta Geologica Sinica - English Edition 78, no. 3 (September 7, 2010): 676–83. http://dx.doi.org/10.1111/j.1755-6724.2004.tb00182.x.

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Qiming, LI, WU Guanghui, PANG Xiongqi, PAN Wenqin, LUO Chunshu, WANG Chenglin, LI Xinsheng, and ZHOU Bo. "Hydrocarbon Accumulation Conditions of Ordovician Carbonate in Tarim Basin." Acta Geologica Sinica - English Edition 84, no. 5 (October 2010): 1180–94. http://dx.doi.org/10.1111/j.1755-6724.2010.00289.x.

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38

Wu, Lin, Shuwei Guan, Rong Ren, and Chunyu Zhang. "Sedimentary evolution of Neoproterozoic rift basin in northern Tarim." Petroleum Research 2, no. 4 (December 2017): 315–23. http://dx.doi.org/10.1016/j.ptlrs.2017.03.004.

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39

Zhang, Guang-Ya, and Shi-Xia Gao. "Transfer Structures in the Northern Tarim Basin, Northwest China." International Geology Review 38, no. 3 (March 1996): 284–91. http://dx.doi.org/10.1080/00206819709465335.

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40

FENG, Chang-Ge, Shao-Wen LIU, Liang-Shu WANG, and Cheng LI. "Present-Day Geothermal Regime in Tarim Basin, Northwest China." Chinese Journal of Geophysics 52, no. 6 (November 2009): 1237–50. http://dx.doi.org/10.1002/cjg2.1450.

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41

Prudnikova, T. N. "The Tarim Basin and the Transformation of its Landscapes." Arid Ecosystems 9, no. 3 (July 2019): 157–65. http://dx.doi.org/10.1134/s2079096119030089.

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42

Andreev, Plamen S., Wenjin Zhao, Nian-Zhong Wang, Moya M. Smith, Qiang Li, Xindong Cui, Min Zhu, and Ivan J. Sansom. "Early Silurian chondrichthyans from the Tarim Basin (Xinjiang, China)." PLOS ONE 15, no. 2 (February 13, 2020): e0228589. http://dx.doi.org/10.1371/journal.pone.0228589.

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43

Xiong, Yufei, Tianqing Chen, Gang Li, and Zhijie Ta. "Study on Water Transfer in Low Tarim River Basin." IOP Conference Series: Materials Science and Engineering 394 (August 7, 2018): 052046. http://dx.doi.org/10.1088/1757-899x/394/5/052046.

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44

Liu, Yan, and Yanghua Wang. "Seismic characterization of a carbonate reservoir in Tarim Basin." GEOPHYSICS 82, no. 5 (September 1, 2017): B177—B188. http://dx.doi.org/10.1190/geo2016-0517.1.

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Seismic characterization of carbonate reservoirs is a challenging task for geophysicists because of their special depositional environment and complex interior structures. We developed a case study of the seismic characterization of a karstified carbonate reservoir in the Tarim Basin, western China. The characterization procedure is sequential and includes fault and fracture detection, seismic facies classification, seismic impedance inversion, and lithofacies classification. We presented a dip-steered coherence algorithm for detecting faults and karst fractures in the carbonate reservoir. Incorporating the dip information improves the performance and robustness. We applied normalized seismic segments, rather than the amplitude values, as the input to seismic facies classification, so as to reduce the impact of strong amplitudes, such as karst fractures, and to enable the analysis of weak amplitudes in the background strata. For the impedance inversion, we adopted a Fourier integral method for fast simulation in the stochastic inversion in this karstified carbonate reservoir. The algorithm honors the lateral variation based on the seismic trace similarity, instead of the lateral variogram that is commonly used in stochastic inversion. We conducted lithofacies classification, in which we used seismic coherence as a prior knowledge, so as to honor the fracture-associated local lithofacies with dolomitization and to distinguish it from limestone without dolomitization. Based on reservoir characterization described above, we determined three drilling wells for potential oil/gas exploration.

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45

达, 朝吉. "Analysis of Runoff Evolution Law of Tarim River Basin." Journal of Water Resources Research 01, no. 05 (2012): 353–58. http://dx.doi.org/10.12677/jwrr.2012.15054.

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46

Guo, Ning, Chao Wu, and Stuart Fagin. "Seismic imaging of complex structures in the tarim basin." Journal of Earth Science 26, no. 4 (July 25, 2015): 586–91. http://dx.doi.org/10.1007/s12583-015-0560-9.

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47

Song, Yudong, Ranghui Wang, and Yongsheng Peng. "Water resources and ecological conditions in the Tarim Basin." Science in China Series D: Earth Sciences 45, S1 (December 2002): 11–17. http://dx.doi.org/10.1007/bf02878383.

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48

Yuzhu, Kang, and Kang Zhihong. "Tectonic evolution and oil and gas of Tarim basin." Journal of Southeast Asian Earth Sciences 13, no. 3-5 (March 1996): 317–25. http://dx.doi.org/10.1016/0743-9547(96)00038-4.

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Sproat, Colin D., and Renbin Zhan. "Altaethyrella (Brachiopoda) from the Late Ordovician of the Tarim Basin, Northwest China, and its significance." Journal of Paleontology 92, no. 6 (July 6, 2018): 1005–17. http://dx.doi.org/10.1017/jpa.2018.31.

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AbstractAltaethyrella tarimensis, a new species of rhynchonellide brachiopod, is described from the late Katian (Late Ordovician) Hadabulaktag Formation in the Kuruktag region of Xinjiang, Northwest China on the northeastern edge of the Tarim Basin. Serial sections of the shell clearly show no dorsal median septum or septalium in the dorsal valve, and no spiralia or atrypide-style crura. Like other species of the genus, A. tarimensis n. sp. exhibits a high degree of intraspecific variation, including variations in shell shape and size, number of ribs in the sulcus at the anterior, and degree of asymmetry. The discovery of Altaethyrella in Tarim has important paleogeographic implications, indicating a close relationship between the Late Ordovician brachiopod faunas of Tarim and those of the Kazakh terranes and North and South China paleoplates, supporting a recently published paleogeographic projection that places Tarim near the Chu-Ili terrane during the Late Ordovician. The abundant large biconvex shells of A. tarimensis n. sp. would have provided a firm substrate for encrusting filter feeders like bryozoans to establish on the Kuruktag Platform.UUID: http://zoobank.org/df8843cd-4db0-48e7-ba03-bf0ce81c4f01

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Xiao, Zong Lin, Qing Qing Hao, and Zhong Min Shen. "Maturity Evolution of the Cambrian Source Rocks in the Tarim Basin." Advanced Materials Research 622-623 (December 2012): 1642–45. http://dx.doi.org/10.4028/www.scientific.net/amr.622-623.1642.

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The Tarim basin is an important petroleum basin in China, and the Cambrian strata are the major source rock successions in the basin. Integrated the source rock depositional and structural history with its geochemical and thermal parameters, this paper simulates the evolution of the Cambrian source rocks with the software Basinview. The simulation result shows that the main hydrocarbon-generation centers of the Manjiaer sag in the Tabei depression and the Tangguzibasi sag in the Southwest depression are characterized by their early hydrocarbon generation, and in the late Ordovician depositional age, they reached dry gas stage. The Kuqa and Southwest depressions developed in the Cenozoic foreland basins made the Cambrian source rocks mature rapidly in the Cenozoic period. The source rock maturity in the Tarim basin now is characterized by high in the east and west and low in the middle, and most of the area is in the over-mature stage in the present. This study can provide available maturity data for the next petroleum exploration work.

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Journal articles on the topic 'Tarim Basin'

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