Pleistocene melting and rapid exhumation of the Nanga Parbat massif, Pakistan: age and P-T conditions of accessory mineral growth in migmatite and leucogranite
Rapid Pleistocene exhumation of the core of the Nanga Parbat massif (northwestern Himalayan syntaxis) is inferred by combining U-Pb dates from monazite, xenotime, and zircon from migmatitic rocks and a leucogranite dike with pressure estimates that are closely linked to dated events in the melting a...
Príomhchruthaitheoirí: | , , , |
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Formáid: | Journal article |
Teanga: | English |
Foilsithe / Cruthaithe: |
Elsevier
2009
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Ábhair: |