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,...

Full description

Saved in:
Bibliographic Details
Published inTectonophysics Vol. 328; no. 1; pp. 1 - 14
Main Author Brookfield, M.E.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 20.12.2000
Subjects
Online AccessGet full text

Cover

Loading…