Role of alternating redox conditions in the formation of organic-rich interval in the Middle Devonian Marcellus Shale, Appalachian Basin, USA-Reference-Cited by-同舟云学术

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Role of alternating redox conditions in the formation of organic-rich interval in the Middle Devonian Marcellus Shale, Appalachian Basin, USA

Published:2016-03 Issue: Volume:446 Page:85-97
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Chen Ruiqian,Sharma Shikha

Funder

National Science Foundation

National Energy Technology Laboratory's Regional University Alliance

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference140 articles.

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2. Mo–total organic carbon covariation in modern anoxic marine environments: implications for analysis of paleoredox and paleohydrographic conditions;Algeo;Paleoceanography,2006

3. Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems;Algeo;Chem. Geol.,2004

4. Trace-metal covariation as a guide to water-mass conditions in ancient anoxic marine environments;Algeo;Geosphere,2008

5. Paleoceanographic applications of trace-metal concentration data;Algeo;Chem. Geol.,2012

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