Multi‐target‐oriented seismic exploration in desert area of Tarim Basin ‐ A case history

Author(s):  
Wang Xinquan ◽  
Yan Feng ◽  
Duan Mengchuan ◽  
Gao Guocheng ◽  
Zhong Hai
2010 ◽  
Vol 2010 (1) ◽  
pp. 1-3
Author(s):  
Jian Guo ◽  
Diandong Zhao

2015 ◽  
Author(s):  
Qiang Li ◽  
Ruiying Liu ◽  
Peng Kang ◽  
Guofeng Xia ◽  
Xingwang Zhang ◽  
...  

2021 ◽  
Author(s):  
Peng Gengxin ◽  
Duan Mengchuan ◽  
Xu Kaichi ◽  
Zhu Yunhong ◽  
Pei Guangping ◽  
...  

2009 ◽  
Vol 52 (4) ◽  
pp. 803-813 ◽  
Author(s):  
Nan-Sheng QIU ◽  
Peter Reiners ◽  
Qing-Hua MEI ◽  
Guang JIANG ◽  
Nicolesco Stefan ◽  
...  

2003 ◽  
pp. 110-126 ◽  
Author(s):  
Brian Roberts ◽  
Eva Zaleski ◽  
Gervais Perron ◽  
Erick Adam ◽  
Larry Petrie ◽  
...  

2016 ◽  
Vol 4 (3) ◽  
pp. T337-T346 ◽  
Author(s):  
Yang Ping ◽  
Sun Longde ◽  
Qi Jiafu

The Kuqa area of the Tarim Basin is a typical foreland thrust belt. Abundant petroleum resources are stored in the complex subsalt structures at depths greater than 6500 m. The extremely rugged surface, the severely deformed gypsum-salt cap above the reservoir, and the large burial depth of the overthrust target make it difficult to accurately delineate the target structures. Those geologic challenges translate into geophysical difficulties of complex seismic wavefields, low signal-to-noise ratio (S/N), and poor imaging accuracy, which compound the exploration challenge in the Kuqa area. To meet the exploration challenge, a research campaign has been conducted since 2005 to integrate seismic acquisition, processing, and interpretation. After almost a decade of research effort and pilot applications, a set of techniques, comprised of wide-line large-array acquisition, anisotropic prestack depth migration under rugged topography, complex structure modeling, and structure mapping with varying velocities, was developed. The use of these techniques has much improved the S/N, imaging accuracy, subsequent interpretation, and well placement. As a result, the success ratio of exploration drilling has increased from less than 25% to more than 64% in the Kuqa area of the Tarim Basin.


2018 ◽  
Vol 55 (12) ◽  
pp. 1384-1388
Author(s):  
Youjun Wang ◽  
Jia Jia ◽  
Hao Liu ◽  
Hao Lu ◽  
Caichen Lu ◽  
...  

The vast desert area of the Tarim Basin contains a large amount of loose sediment, and consequently, it is one of the most important sources of aeolian dust in the mid-latitudes of the Northern Hemisphere. However, only limited research has been undertaken on the provenance of the desert sediments. In this study, we investigated the iron mineralogy including magnetic (Mt), hematite (Hm), and goethite (Gt) characteristics of desert sediments from the Tarim Basin and used them to determine their provenance. The results show that the sediments are characterized by a high content of Gt that comprises up to 0.16, 0.45, and 0.99 wt.% of the 31–63, 8–31, and 2–8 μm fractions, respectively. In contrast to Hm and Mt, Gt is significantly enriched in the fine particle size fraction. Consequently, we propose that the desert sediments originate in a cold and humid environment, which favors the formation of Gt and limits the formation of Mt and Hm. The surrounding high mountains appear to be the only location within this vast region with the climatic conditions favoring Gt formation.


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