Tectonic-thermal Evolution Characteristics of Permian Mud Shale in Panxie Mining Area of Huainan
Received date: 2014-02-13
Revised date: 2015-04-07
Online published: 2015-09-10
Burial history,tectonic-sedimentary history of Panxie mining area in Huaina area,thermal evolution history of Permian mud shale since Late Paleozoic are reconstructed by the vitrinite reflectance geothermometer and paleo-heat flow method.The geological significance of hydrocarbon generation from Permian mud shale is discussed.The results show that the Permian experienced the stable sedimentary stage in the Early Permian-late stage of Middle Jurassic,the rapid uplift from the early stage of Late Jurassic to Late Cretaceous,the re-deposit from the Early Paleocene to the Middle-Late Paleocene,the stable uplift from the Middle-Late Paleocene to the Late Neogene,and the slow deposit since Early Pleistocene in the study area.The geothermal evolution of basin is consistent with the course of the burial-sedimentary history,the paleo-heat flow experienced stable stage from Permian to Late-Jurassic,the drastic decrease from the end of Late Jurassic to the end of Paleogene and the subsequent smoothly stabilization.Permian source rocks enter the early to middle-late stage at the mature stage from the Middle-Late Permian to the Middle Jurassic,and the maturation ended in the end of Late Permian.The formation of shale gas includes four stages such as the generation of bacterial gas and thermogenic gas from Early Permian to Late Jurassic,the replenishment and the whole tectonic destruction of gas reservoir from Late Jurassic to Late Cretaceous,the generation of bacterial gas and thermogenic gas in some Paleogene strata,the second tectonic destruction of gas reservoir from Late Paleogene to Early Quaternary.The burial and uplift periods of Permian from different boreholes are consistent.There is a little difference in the sedimentary and uplift degree.The thermal evolution degree is caused by the subtle difference from the sedimentary degree and the uplift-erosion rate,but the hydrocarbon generation from different boreholes is generally consistent.
LIU Hui-hu，HU Bao-lin，XU Hong-jie，ZHANG Wen-yong，ZHENG Kai-ge，CHENG Qiao . Tectonic-thermal Evolution Characteristics of Permian Mud Shale in Panxie Mining Area of Huainan[J]. Natural Gas Geoscience, 2015 , 26(9) : 1696 -1704 . DOI: 10.11764/j.issn.1672-1926.2015.09.1696
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