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Metamorphic Densification in Greater India by ms827291129 is a document available to read on EtoBox.
The study investigates the missing felsic crust of the Greater Indian continent, revealing that approximately 20-47% of it is absent due to metamorphic densification during the India-Asia collision. The research employs phase equilibria modeling to demonstrate that the density of the felsic crust becomes greater than the surrounding mantle under high pressure, enabling spontaneous subduction. This process contributes to the rapid convergence of the Indian and Asian plates and explains the observed crustal ma
- Author
- ms827291129
- Language
- EN