It is located in China . [6][3], In addition, at some distances further away from the North Qinling Belt, a continental arc with volcanoes was formed at another subducting plate boundary as well, which is named the Proto-Erlangping arc. [29] Limestone, Shale, sandstone and other sedimentary rocks were deposited on top of basement rocks at the Paleozoic (545-250 million years ago), with a minor amount of sandstone deposited until the Triassic period (205 million years ago). Add a photo to this gallery. [20] It was first formed 1000 million years ago by magmatic activities which occurred in an oceanic-arc environment. [3][18], At the early Cambrian (around 540 million years ago), Gondwana (considered as super-continent by some geologists) started to develop. [6][22] What different was the subducting plate changed from one to another, at the Danfeng island. Early Cretaceous to late Cretaceous (140 to 83 million years ago). [3][6] An arc can be formed because the subducted lower plate melted in the mantle and rose up to the opposite upper plate while cutting through lines of weakness of plate. The Qinling Mountains is a place seen in season seven. This section lacks information. [3][18] By the time the North Qinling Belt moved away from Rodinia, it was colliding with the Proto-Erlangping arc as well. Abhängig von der Höhenlage sind die Tiere in verschiedenen Vegetationstypen anzutreffen. English [] Proper noun []. [6][17][24] Resulting from extremely strong compressional force, all individual blocks were shortened horizontally but thickened vertically. [3], On the other hand, the formation of North Qinling belt was more complicated. At this time North and South Qinling belt were still aligning next to each other, therefore they shared the same Shangdan ocean. The North Qinling Group, one of the major block that built up the Qinling orogen, is characterized by gneiss, amphibolite and marble which were metamorphosed from clastic sedimentary rock and carbonate. The Qinling Mountains (Traditional Chinese: 秦嶺, Simplified Chinese: 秦岭) are a major mountain range. It did not initially exist with North China Block, but a part of super-continent Rodinia. The Qinling Mountains is covered by large scale plants, which are home to many wild animals such as giant pandas and golden monkeys. A stable population of the Giant panda is found in the Foping National Nature Reserve in the ecoregion.
The Qinling Huaihe line was first drawn by Chinese geographer Zhang Xiangwen in 1908, defining north China as anything above a line running along the Qinling Mountains in the west and the Huai River the east. Overview. [27][28] As a result, right-lateral strike slip fault became dominated. [9][10][13] Until the late Cretaceous (83 million years ago), the Qinling complex was affected by a WNW-ESE extension event in west of Qinling. [8] It can be divided into 9 main groups: South-North China Block, Kuanping Group, Erlangping Group, North Qingling Block, Shangdan suture zone, North-South Qinling Block, South-South Qinling Block, Mianlue Suture zone and Dabie terrane. [3][18], A similar process occurred at the North Qinling belt, North Qinling belt and Rodinia were separated. [3] An island arc called 'DanFeng island arc' was formed. [28][27] At the late Pliocene (3.5 million years ago), left-lateral strike-slip fault dominated the Qinling, which was caused by a NNW-SSE extension event until the Present. [3][6], At late Cambrian (around 500 million years ago), the North China block migrated closer to North Qinling block. [19] Then, magma cooled down and became rocks which contribute to the major basement of the South Qinling belt. Ophiolites were formed during early Cambrian to Early Silurian (545 to 423 million years ago). You can help Winx Club Wiki by expanding it.
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