Structures of dolomite at ultrahigh pressure and their influence on the deep carbon cycle
Structures of dolomite at ultrahigh pressure and their influence on the deep carbon cycle
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United States: National Academy of Sciences
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Language
English
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Publisher
United States: National Academy of Sciences
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Contents
Carbon-bearing solids, fluids, and melts in the Earth's deep interior may play an important role in the long-term carbon cycle. Here we apply synchrotron X-ray single crystal micro-diffraction techniques to identify and characterize the high-pressure polymorphs of dolomite. Dolomite-II, observed above 17 GPa, is triclinic, and its structure is topo...
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Full title
Structures of dolomite at ultrahigh pressure and their influence on the deep carbon cycle
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TN_cdi_proquest_miscellaneous_1803148968
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1803148968
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ISSN
0027-8424
E-ISSN
1091-6490
DOI
10.1073/pnas.1201336109
