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- W2356170125 abstract "Simultaneously with the colliding of the North China plate and Yangtze plate along the Shang-dan suture zone in the late Caledonian,a nearly east-west-trending extensional belt was initiated on the northern margin of the Yangtze plate,i.e.the present South Qinling tectonic belt.The belt is composed of the extensional tectonics of the Wudang block,Paleozoic basic sheet swarms in the Wudang block and Ziyang-Langao Paleozoic alkaline magmatic zone,Zhen'an-Xunyang Devonian shallow rift basin and Fop-ing uplift.This extensional belt formed between two collision events in terms of time and between the north and south sutures of the Qinling orogen in terms of space;so the extension represents a very im-portant evolutional stage.The authors propose that the initiation of the extension is very likely to be relat-ed to the gravitational collapse of the orogenic belt caused by collision of the South Qinling and North Qinling belts.Along with the formation of the Late Pale ozoic Mianlue ocean south of this extensional belt,South Qinling gradually evolved into a passive continent margin on the south side of the North China plate.Therefore the crustal extension of the South Qinling lasted to the Early -Mid Triassic.The geochronology and geochemistry of the basic sheets intruded along the bedding into the extensional detach-ment system of the Wudang block during the extension suggest that they have many similarities to those of metadiabase and metabasic volcanic rocks of the Mianlue ophiolite;so it is very possible that the Mianlue ocean is the result of this extension of the South Qinling." @default.
- W2356170125 created "2016-06-24" @default.
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- W2356170125 date "2002-01-01" @default.
- W2356170125 modified "2023-09-28" @default.
- W2356170125 title "Mid-Late Paleozoic extension of the Wudang block in the South Qinling tectonic belt,China" @default.
- W2356170125 hasPublicationYear "2002" @default.
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