Mesozoic intracontinental orogeny in the Qinling Mountains, central China
Abstract
null null The Qinling Orogenic belt has been well documented that it was formed by multiple steps of convergence and subsequent collision between the North China and South China Blocks during Paleozoic and Late Triassic times. Following the collision in Late Triassic times, the whole range evolved into an intracontinental tectonic process. The geological, geophysical and geochronological data suggest that the intracontinental tectonic...
Paper Details
Title
Mesozoic intracontinental orogeny in the Qinling Mountains, central China
Published Date
Feb 1, 2016
Journal
Volume
30
Pages
144 - 158
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