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- W2366421432 abstract "The Junggar orogenic belt in Xinjiang is a polycyclic orogenic belt between the Siberian conti-nental crust and Tarim continental crust as well as a main part of the Paleo-Asian Ocean.This orogenic belt broke up and expanded into an ocean on the basement of the craton formed in the early Neoprotero-zoic.Its development progressed through polycyclic accordion-style opening-closing movement(when one part opened the other part closed,and the head was connected with the tail)and multiple transformations of land and sea,and finally a number of trench-arc-basin systems were amalgamated and consolidated into a new Paleo-Asian continent at the end of the Carboniferous.After the formation of the continent,it was not stable;strong activity and orogeny still continued during the Meso-Cenozoic.The manifestations in-clude poly-epochal ophiolite and orogenic granite and different types of orogeny." @default.
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- W2366421432 date "2004-01-01" @default.
- W2366421432 modified "2023-09-26" @default.
- W2366421432 title "Characteristics of polycyclic opening-closing tectonics in the J unggar orogenic belt ,Xinjiang" @default.
- W2366421432 hasPublicationYear "2004" @default.
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