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Basinal marine dolomicrite from the Pennsylvanian/Wolfcampian Horquilla Formation, New Mexico
Year:
1989
Source of publication :
Journal of Sedimentary Petrology
Authors :
Graber, Ellen
;
.
Volume :
59
Co-Authors:
Graber, E.R., Dept. of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA.
Lohmann, K.C., Dept. of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA.
Facilitators :
From page:
4
To page:
12
(
Total pages:
9
)
Abstract:
Deep-water lithologic associations, absence of hypersaline and freshwater indicators, elevated Na and Sr contents, and marine-derived delta 18O values all indicate that the dolomite precipitated from marine-derived water during burial beneath the sediment-water interface. Depletion of sulfate was not a prerequisite for dolomitization of basinal carbonates of the Horquilla Formation. Rather, dolomitization was promoted by the metastability of the precursor mineralogy. -from Authors
Note:
Related Files :
burial
Deep Sea Drilling Project
dolomicrite
Horquilla Formation
Permian
USA, New Mexico
Wolfcampian
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Related Content
More details
DOI :
10.1306/212F8F03-2B24-11D7-8648000102C1865D
Article number:
Affiliations:
Database:
Scopus
Publication Type:
Language:
English
Editors' remarks:
ID:
19834
Last updated date:
02/03/2022 17:27
Creation date:
16/04/2018 23:31
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Scientific Publication
Basinal marine dolomicrite from the Pennsylvanian/Wolfcampian Horquilla Formation, New Mexico
59
Graber, E.R., Dept. of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA.
Lohmann, K.C., Dept. of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA.
Basinal marine dolomicrite from the Pennsylvanian/Wolfcampian Horquilla Formation, New Mexico
Deep-water lithologic associations, absence of hypersaline and freshwater indicators, elevated Na and Sr contents, and marine-derived delta 18O values all indicate that the dolomite precipitated from marine-derived water during burial beneath the sediment-water interface. Depletion of sulfate was not a prerequisite for dolomitization of basinal carbonates of the Horquilla Formation. Rather, dolomitization was promoted by the metastability of the precursor mineralogy. -from Authors
Scientific Publication
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