Geological development and Phanerozoic crustal accretion in the western segment of the southern Tien Shan (Kyrgyzstan, Uzbekistan and Tajikistan)
The Tien Shan form a high intracontinental mountain belt, lying north of the main India-Asia collision mountains, and consist of re-activated Paleozoic orogens. The western segment of the southern Tien Shan lies northwest of the Pamir and west of the Talas–Fergana fault. The stratigraphy, lithology,...
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Published in | Tectonophysics Vol. 328; no. 1; pp. 1 - 14 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
20.12.2000
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Subjects | |
Online Access | Get full text |
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