supported by the National Natural Science Foundation of China(Grant Nos.91962109,42174094);the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(Grant No.2019QZKK0701);the Fund of Chinese Geological Survey(Grant No.DD20190016);the Basic Scientific Research Fund of the Institute of Geology,Chinese Academy of Geological Sciences(Grant No.J2015)。
The North Himalayan gneiss domes(NHGD),as one of the extensional structures widely distributed across the southern Tibetan Plateau,are an important window for studying post-collisional diastrophism and magmation as we...
Bangladesh is a country with limited sources of energy and since 1990 natural gas has been its main source of energy. Most of the exploration approaches had been conducted onshore especially in the central and eastern...
Mangerak salt diapir is in the South West of Firuz Abad in Fars province, southern Iran and structurally, it is exposed in the simple folded belt of Kohzad Zagros. This diapir, now, is located in a transtentional zone...
supported by the National Natural Science Foundation of China (No. 41272121);the Major National Science and Technology Programs in the "Twelfth Five-Year" Plan of China (No. 2011ZX05025-002-02-02);the Fundamental Research Funds for the Central Universities (No. 16CX02038A)
The Qiongdongnan Basin(QDNB) is situated in the extensional zone at the vertex of the V-shaped northwest sub-basin, non-volcanic northern margin of the South China Sea(SCS). From north to south, the thickness of t...
supported by the National Natural Science Foundation of China under contract No.40002015;the Chinese Academy of Sciences under contract No.KZCX1-07.
Many growth faults developed in the Dongying sag of the Jiyang depression of the Bohai Gulf basin, China. These normal growth faults consist of flower-like grabens in the hanging walls of the major faults, accompanied...
This project was supported by the National Natural Science Foundation of China (Grant No.40125008) and 973 Project (Grant No. 1999043309).
The diapirism in the Yinggehai Basin is a combined result of strong overpressure caused by rapid sedimentation of fine-grain sediments and the tensile stress field resulting from right-lateral slip of the boundary-fau...
Overpressure developed throughout most of the Yinggehai basin. The burial depth to top overpressure varied from about 1 600 m to 4 500 m, with the shallowest top overpressure occurring in the depocenter. The main caus...