financial support for this work comes from the Science Foundation of CUPB(No.2462017YJRC023);supported by the Exploration and Development Research Institute of Petro China Tarim Oilfield Branch Company
The tight sandstone in the Tarim Basin has the characteristics of large burial depth and development of nature fractures due to concentrated in-situ stress. Identifying the present-day in-situ stress orientation is im...
This work was supported by the National Key Research and Development Project(No.2019YFC0605501);the National Science and Technology Major Project(2016ZX05003001).
The buried depth of the gas-producing reservoir in the Kuqa foreland thrust belt of the Tarim Basin exceeds 6000 m.The average matrix porosity of the reservoir is 5.5%,and the average matrix permeability is 0.128×10^...
supported by the National Natural Science Foundation of China (Grant No.41302094);the Petro China Innovation Foundation (Grant No.2012D-5006-0109)
The Cretaceous Bashijiqike Formation is the main gas-bearing strata in the northern structural deformation zone of Kuqa subbasin. The acidic dissolution of this formation arose at 5-4Ma, which corresponds to the late ...
supported by the Ministry of Science and Technology of China(Grant No.G1999043304);the National Natural Science Foundation of China(Grant No.40372056).
The Cretaceous system of the Kuqa depression is a regional scale (second order) depositional sequence defined by parallel unconformities or minor angular unconformities. It can be divided into four third-order sequenc...