Formation and Geochemistry of Precambrian Cherts
Abstract
Cherts, specifically null Precambrian null cherts, are fine-grained rocks consisting dominantly or entirely of SiO 2 null in the form of microcrystalline quartz, subordinate megaquartz, and (rarely) chalcedonic quartz. Cherts may be chemical precipitates, or they may be replacements of preexisting carbonates, volcanoclastic sediments, or igneous and metamorphic...
Paper Details
Title
Formation and Geochemistry of Precambrian Cherts
Published Date
Jan 1, 2007
Journal
Pages
1 - 21
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