A synvolcanic origin for magnetite-rich orebodies hosted by BIF in the Weld Range District, Western Australia
Abstract
Iron ore deposits hosted by Archean banded iron-formation (BIF) in the Weld Range greenstone belt are representative of most of the documented iron ore deposits in the Yilgarn Craton. They include near-surface, supergene goethite-hematite orebodies that overlie and partly modify deeper occurrences of hypogene magnetite and specular hematite ores. The Cenozoic goethite-hematite-rich orebodies in these deposits are unequivocally the product of...
Paper Details
Title
A synvolcanic origin for magnetite-rich orebodies hosted by BIF in the Weld Range District, Western Australia
Published Date
Feb 1, 2018
Journal
Volume
93
Pages
211 - 254
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