Discussion on Sedimentary Environments,Origin and Source of Middle Permian Gufeng Formation Bedded Cherts in theNorthern Margin of the Middle-Lower Yangtze Area
Received date: 2019-09-29
Revised date: 2019-12-20
Online published: 2020-03-24
Supported by
the National Natural Science Foundation of China "Large-scale accumulation of oil and gas during unidirectional cracking-convergence in the Tethys region"(91755211);The National Science and Technology Major Project "Distribution law and exploration evaluation of large and medium oil and gas fields of Marine carbonate"(2017ZX05005-001)
Cherts contain important information of paleogeography, paleostructure and paleo-ocean, which is the important means of studying petrotectonics. With regard to the major disputes on the sedimentary environments, origin and source of Gufeng Formation bedded cherts in the northern margin of middle-lower Yangtze area, demonstrations from both forward and reverse aspects from the perspective of the sedimentary-tectonic evolution were given. By summarizing previous views on the genesis of bedded cherts in Gufeng Formation, and extensively collecting published original geochemical data, in the forward demonstrations we created the database of the cherts about rare earth elements to systematically identify the sedimentary environments, origin and source of cherts. By sorting out the time and cause of the main geological events in the middle Permian in south China, in the reverse demonstrations we established the sequence of tectonic evolution to verify or explain the current series of disputes. The results show that:
Zhenyang Zhao , Shuangjian Li , Genhou Wang . Discussion on Sedimentary Environments,Origin and Source of Middle Permian Gufeng Formation Bedded Cherts in theNorthern Margin of the Middle-Lower Yangtze Area[J]. Advances in Earth Science, 2020 , 35(2) : 137 -153 . DOI: 10.11867/j.issn.1001-8166.2020.003
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