funded by the Major Project of the Changqing Oilfield‘Research on the Tectonic,Sedimentary,Mechanism and New Exploration of the Mesoproterozoic Changcheng System in the Ordos Basin’(ZDZX2021);the National Natural Science Foundation of China(42241204,42073054);the Fundamental Research Funds for the Central Universities,CHD(300102272205,300102272207).
The present-day pressure pattern is the ultimate result of the evolution of paleo-pressure,so understanding the variation of stress throughout geological history is of great significance for oil and gas accumulation.I...
supported by the National NaturalScience Foundation of China(Grant No.41802163,41503033);Hunan Provincial Natural Science Foundation of China(Grant No.2018JJ3152);the Science and Technology Plan Project of Sichuan province(Grant No.2018JZ0003);the State Petroleum and Gas Specific Project(Grant No.2016ZX05061001-001)
Nanoscale pore characteristics of the Upper Permian Longtan transitional mudrocks and their equivalent strata Wujiaping Formation marine mudrocks in and around the eastern Sichuan Basin was investigated using field em...
The podiform chromitites in the Luobusa ophiolite, Southem Tibet, have received much attention because of the presence of ultrahigh-pressure minerals, such as micro- diamonds (Bai et al., 1993; Yang et al., 2007; Xu ...
This research was supported by the National Natural Science Foundation of China
According to the kinds of feldspar and rock associations in the Ai-rich gneisses, the low-pressure metamorphic crust of the Early Proterozoic granulite facies in central Inner Mongolia can be divided into southern and...