Metamorphic CO2 production in calc-silicate rocks from the eastern Himalaya
Abstract
The Tibetan Plateau is one of the most geologically dynamic systems and the highest plateau in the world with ongoing three-dimensional crustal deformation. The Plateau is uplifting and deforming horizontally as observed by present-day global navigation satellite system (GNSS) and repeated leveling measurements. Crustal mass is conservative and less dense than the mantle, thus the horizontal shortening must be accompanied by crustal thickening...
Paper Details
Title
Metamorphic CO2 production in calc-silicate rocks from the eastern Himalaya
Published Date
Feb 1, 2017
Volume
136
Issue
1
Pages
39 - 49
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