With the analysis of the gastesting data, the Upper Paleozoic reservoir temperature in Yanchang area has been calculated. Based on thermal evolution indicators and palaeogeothermal recovery, it is indicated that the Upper Paleozoic source rocks have reached the maturity stage and the overmaturity stage. The paleogeothermal gradient in different period is discussed. The erosion thickness of the formation in this region was recovered. The thermal evolution history of Upper Paleozoic in Yanchang exploratory area has been reproduced. The main sedimentation period is Late Triassic(226~208Ma). The Upper Paleozoic source rocks reached the maturity stage in Early Jurassic and reached the high maturity stage in Late Jurassic. The main gas generation period of the Upper Paleozoic in Yanchang area is from Late Jurassic to Early Cretaceous.
参考文献
相似文献
引证文献
引用本文
于强,任战利,王宝江,高利军,李成福,曹红霞.2012.鄂尔多斯盆地延长探区上古生界热演化史[J].地质论评,58(2):303-308,[DOI]. .2012. Thermal Evolution History of the Upper Paleozoic in Yanchang Exploratory Area, Ordos Basin[J]. Geological Review,58(2):303-308.