Petrographic and geochemical characteristics of dolomite types and the origin of ferroan dolomite in the Trenton Formation, Ordovician, Michigan Basin, U.S.A.

Sedimentology

Volumn 33, Issue 1, 1986, Pages 61-86

  TAYLOR, THOMAS R ^a   SIBLEY, DUNCAN F ^a  

^a MICHIGAN STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0022506027     PISSN: 00370746     EISSN: 13653091     Source Type: Journal    
DOI: 10.1111/j.1365-3091.1986.tb00745.x     Document Type: Article

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5. Sedimentary pyrite formation
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7. Authigenic iron sulfides as palaeosalinity indicators
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13. Thermal history of Michigan Basin
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21. Magnesium‐iron replacement in clay minerals in anoxic marine sediments
22. Structural and compositional variations in some natural dolomites
23. 3:1) Phase relations, 2) a method for major element spectrochemical analysis. 3) composition of some ferroan dolomites
24. Removal of magnesium from interstitial waters in reducing environments: the problem reconsidered
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27. Isotopic evidence for source of diagenetic carbonates formed during burial of organic‐rich sediments
28. Early diagenetic precipitation and pore fluid migration in the Kimmeridge clay of Dorset, England
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47. 3 between 350 and 550°C
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51. Petrographic and geochemical characteristics of dolomite types and the origin of ferroan dolomite in the Trenton Formation, Michigan Basin
52. Burial cementation in the Devonian Kaybob Reef Complex, Alberta, Canada