Structure of the Panzhihua intrusion and its Fe-Ti-V deposit, China
Abstract
The Panzhihua intrusion in southwest China is part of the Emeishan large igneous province and host of a large Fe-Ti-V ore deposit. In previous interpretations it was considered to be a layered, differentiated sill with the ore deposits at its base. New structural and petrological data suggest instead that the intrusion has an open S-shape, with two near-concordant segments joined by a discordant dyke-like segment. During emplacement of the main...
Paper Details
Title
Structure of the Panzhihua intrusion and its Fe-Ti-V deposit, China
Published Date
Sep 1, 2013
Journal
Volume
4
Issue
5
Pages
571 - 581
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