Correlation between magmatism of the Ladakh Batholith and plate convergence rates during the India–Eurasia collision
Abstract
Evidence for episodic magmatism is found within large batholiths of ancient and modern convergent margin settings and is often attributed to regional geodynamic changes such as an increase in plate convergence rate, lithospheric extension and/or delamination, and intra-crustal/lithospheric shortening. The nature and timing of collision between India and Eurasia remain contentious as many models suggest that the “hard” collision occurred during...
Paper Details
Title
Correlation between magmatism of the Ladakh Batholith and plate convergence rates during the India–Eurasia collision
Published Date
Nov 1, 2014
Journal
Volume
26
Issue
3-4
Pages
1051 - 1059
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