TTG-type plutonic rocks formed in a modern arc batholith by hydrous fractionation in the lower arc crust
We present the geochemistry and intrusion pressures of granitoids from the Kohistan batholith, which represents, together with the intruded volcanic and sedimentary units, the middle and upper arc crust of the Kohistan paleo-island arc. Based on Al-in-hornblende barometry, the batholith records intr...
| Main Authors: | , , , , , |
|---|---|
| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
Springer Berlin Heidelberg
2016
|
| Online Access: | http://hdl.handle.net/1721.1/105386 https://orcid.org/0000-0003-2402-3736 |