Melting of carbonate wall rocks and formation of the heterogeneous aureole of the Panzhihua intrusion, China
Abstract
The Panzhihua gabbroic intrusion, part of the plumbing system of the Emeishan large igneous province, intruded late-Proterozoic dolomites and marls about ∼263 Ma ago. The dolomites in the contact aureole were converted to brucite marbles and a diverse suite of forsterite, diopside and garnet skarns. The variation in mineralogy is explained in part by differences in the composition of the protolith, particularly the proportion of silica minerals...
Paper Details
Title
Melting of carbonate wall rocks and formation of the heterogeneous aureole of the Panzhihua intrusion, China
Published Date
Sep 1, 2013
Journal
Volume
4
Issue
5
Pages
535 - 546
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Notes
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