Burial history and thermal evolution characteristics of source rocks of the Upper Triassic Xujiahe Formation, Sichuan Basin
LI Ya
Abstract
LI Ya
Abstract
According to the geologial data and the present geothermal and paleogeothermal data from 52 exploration wells, the authors analyzed the changes of burial history,maturity evolution and thermal history, and gas generation with time of each well with PetroMod software. The results show that the Upper Triassic source rocks in northern and middle Sichuan basin came into the oil-generating window in middle and late Jurassic, respectively. However, the Upper Triassic source rocks in southern Sichuan basin entered into hydrocarbon generation threshold in Early Cretaceous. The source rocks continued to be buried at the greatest depth and then reached the oil-generating peak until the late stage of late Cretaceous. After that, Sichuan basin experienced a uplifting process as a whole under the late Yanshanian and Himalayan movements, while the thermal evolution of kerogen was ended eventually.
OpenAlex reports 4 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
According to the geologial data and the present geothermal and paleogeothermal data from 52 exploration wells, the authors analyzed the changes of burial history,maturity evolution and thermal history, and gas generation with time of each well with PetroMod software. The results show that the Upper Triassic source rocks in northern and middle Sichuan basin came into the oil-generating window in middle and late Jurassic, respectively. However, the Upper Triassic source rocks in southern Sichuan basin entered into hydrocarbon generation threshold in Early Cretaceous. The source rocks continued to be buried at the greatest depth and then reached the oil-generating peak until the late stage of late Cretaceous. After that, Sichuan basin experienced a uplifting process as a whole under the late Yanshanian and Himalayan movements, while the thermal evolution of kerogen was ended eventually.
Key concepts: Geology, Source rock, Cretaceous, Kerogen, Structural basin, Geothermal gradient, Paleontology, Sichuan basin