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Formation of dolomite catalyzed by sulfate-driven anaerobic oxidation of methane; mineralogical and...

Formation of dolomite catalyzed by sulfate-driven anaerobic oxidation of methane; mineralogical and...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2038321258

Formation of dolomite catalyzed by sulfate-driven anaerobic oxidation of methane; mineralogical and geochemical evidence from the northern South China Sea

About this item

Full title

Formation of dolomite catalyzed by sulfate-driven anaerobic oxidation of methane; mineralogical and geochemical evidence from the northern South China Sea

Publisher

Washington: Mineralogical Society of America

Journal title

The American mineralogist, 2018-05, Vol.103 (5), p.720-734

Language

English

Formats

Publication information

Publisher

Washington: Mineralogical Society of America

More information

Scope and Contents

Contents

It is very difficult to synthesize dolomite under Earth-surface conditions in the laboratory. However, multiple carbonate phases, including low-Mg-calcite (LMC), high-Mg-calcite (HMC), and dolomite, have been discovered in authigenic carbonate deposits that precipitated at cold methane seeps. The formation of such seep carbonates is triggered by th...

Alternative Titles

Full title

Formation of dolomite catalyzed by sulfate-driven anaerobic oxidation of methane; mineralogical and geochemical evidence from the northern South China Sea

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2038321258

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2038321258

Other Identifiers

ISSN

0003-004X

E-ISSN

1945-3027

DOI

10.2138/am-2018-6226

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