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- W2387468057 abstract "A brief introduction is given to Tectonic map of the eastern Tianshan mountains of Xinjiang in scale 1 : 500000. The tectonic framework and evolution of the eastern Tianshan mountains (ETM) since the early Paleozoic are discussed based on analyses of Paleozoic sedimentary and volcano-sedimentary formations. Tectonically, ETM belongs to plate tectonic system from the Sinian to Devonian periods. From Carbonifeous to Early Permian ETM was shaped by rifting and rift troughs, belonging to post-collisional intra-plate extensional system. During the early-middle stage of Early Paleozoic ETM was a block in the paleo-Asia Ocean as part of the Junggar block. The subsequent accretion to the margin of the Altay paleo-continent led to formation of an accreted margin of Siberian paleo-continent. Due to breakup along the Karamaili from the Silurian to Early Devonian and formation of Karamaili Ocean, ETM separated from Siberian paleo-continent again. Southward subduction of the Karamaili Ocean during Devonian period results in generation of the Dananhu-Tousuquan island arc. Ore-bearing rocks yielding porphyry copper in ETM are composed of island arc complexes. The Karamaili Ocean was closed during the end of Middle Devonian. Post-collisional within-plate extension started since Early carboniferous, accompanied by rifting and formation of rift troughs. Intra-continental orogeny was initiated since Late Permian, and uplift occurred during the Cenozoic due to Indian-Eurasian collision." @default.
- W2387468057 created "2016-06-24" @default.
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- W2387468057 date "2002-01-01" @default.
- W2387468057 modified "2023-09-23" @default.
- W2387468057 title "TECTONICS AND EVOLUTION OF THE EASTERN TIANSHAN MOUNTAINS-A BRIEF INTRODUCTION TO “TECTONIC MAP (1 : 500 000) OF THE EASTERN TIANSHAN MOUNTAINS OF XINJIANG" @default.
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