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- W2393952252 abstract "Based on the results of Geotransect from Dushanzi to Quanshuigou, the crustal structure and tectonics along the profile from Quanshuigou to Altai of Xinjiang were carried out.The transect not only displays the style of basin-mountain tectonics, with three mountain ranges and two basins on the surface, but also reveals different crustal structures in different parts. Furthermore, I recognize that the Tianshan and Qilianshan mountains in western China, belong to orogenic events that occurred in different geological periods, but the recent basin-mountain tectonics are the results of crust-mantle interaction since the Cenozoic. Typically, in the Tianshan Mountains, the Cenozoic orogenic movements were different from those that occured in same area in the Paleozoic, or in the Himalaya in the Cenozoic. I refer to the basin-mountain tectonics as the “Tianshan-type orogenic movements” and “Tianshan-type orogenic zone”." @default.
- W2393952252 created "2016-06-24" @default.
- W2393952252 creator A5016460703 @default.
- W2393952252 date "2006-01-01" @default.
- W2393952252 modified "2023-09-23" @default.
- W2393952252 title "Problems of crustal tectonics and evolution in Xinjiang, Northwest China" @default.
- W2393952252 hasPublicationYear "2006" @default.
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