Feldspar diagenesis in Cambrian clastic rocks of the southern Ozark Mountains and Reelfoot Rift, southeastern Missouri and northeastern Arkansas; implications for mississippi valley-type ore genesis (Q82278): Difference between revisions

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Property / author: Martin Goldhaber / rank
 
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Property / author: Martin Goldhaber / reference
 
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Property / content URL: https://pubs.usgs.gov/bul/1989f/report.pdf / rank
 
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Property / content URL: https://pubs.usgs.gov/bul/1989f/report.pdf / reference
 
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Property / GDDID: 5d2490430b45c76caf9202ad / rank
 
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Property / addresses subject: Characterization of Shale Gas Pore Structure / rank
 
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Property / addresses subject: Characterization of Shale Gas Pore Structure / reference
 
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Property / addresses subject: Machine Learning for Mineral Prospectivity Mapping / rank
 
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Property / addresses subject: Machine Learning for Mineral Prospectivity Mapping / reference
 
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Property / addresses subject: Tectonic and Geochronological Evolution of Orogens / rank
 
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Property / addresses subject: Tectonic and Geochronological Evolution of Orogens / reference
 
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Property / OpenAlex ID: W43448601 / rank
 
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Latest revision as of 03:53, 12 September 2024

Feldspar diagenesis in Cambrian clastic rocks of the southern Ozark Mountains and Reelfoot Rift, southeastern Missouri and northeastern Arkansas; implications for mississippi valley-type ore genesis; 1995; B; 1989-F; Diehl, S. F.; Goldhaber, M. B.
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Feldspar diagenesis in Cambrian clastic rocks of the southern Ozark Mountains and Reelfoot Rift, southeastern Missouri and northeastern Arkansas; implications for mississippi valley-type ore genesis
Feldspar diagenesis in Cambrian clastic rocks of the southern Ozark Mountains and Reelfoot Rift, southeastern Missouri and northeastern Arkansas; implications for mississippi valley-type ore genesis; 1995; B; 1989-F; Diehl, S. F.; Goldhaber, M. B.

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