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- W2375044434 abstract "The study area is located on the northern edge of the Yangtze Block and the south side of the Southern Qinling orogenic belt, and on the west side of this area there are Micang mountain fault belt area and Dabashan arc fault belt area. This area is an overlaying zone between NE and EW trending structure, and it shows great influences on the structure partition, with sensitive re- sponse to tectonic movement in this area. The early study believes that the formations from the Late Permian to the Early Triassic are conformities. However, this study, from the analysis of se- diment formations and structure, identifies the accord unconformity between the middle and the upper Jialingjiang formation (T1-2j2/T1-2j3), which stands for another differential subsidence. The latest effect time of Indosinian movement in this area is early-middle Triassic." @default.
- W2375044434 created "2016-06-24" @default.
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- W2375044434 date "2015-01-01" @default.
- W2375044434 modified "2023-09-23" @default.
- W2375044434 title "Identification of the Accord Unconformity between the Middle and the Upper Jialingjiang Formation and Palaeogeography" @default.
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