An eolian dust origin for clastic fines of Devono-Mississippian mudrocks of the greater North American midcontinent

An eolian dust origin for clastic fines of Devono-Mississippian mudrocks of the greater North American midcontinent—Reply

Published:2024-02-29 Issue:1 Volume:94 Page:156-157
ISSN:1938-3681
Container-title:Journal of Sedimentary Research
language:en
Short-container-title:

Author:

McGlannan Austin J.¹,Bonar Alicia¹,Pfeifer Lily²,Steinig Sebastian³,Valdes Paul³,Adams Steven¹,Duarte David¹,Milad Benmadi¹,Cullen Andrew⁴,Soreghan Gerilyn S.¹

Affiliation:

1. 1 University of Oklahoma, School of Geosciences, Norman, Oklahoma 73019, U.S.A.

2. 2 Rowan University, Department of Geology, Glassboro, New Jersey 08028, U.S.A.

3. 3 University of Bristol, School of Geographical Sciences, Bristol, U.K.

4. 4 Independent Geoscientist, Norman, Oklahoma 73072, U.S.A.

Publisher

Society for Sedimentary Geology

Link

https://pubs.geoscienceworld.org/sepm/jsedres/article-pdf/94/1/156/6283480/i1938-3681-94-1-156.pdf

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3. Boardman, D.R., and Puckette,J. 2006, Stratigraphy and paleontology of Upper Mississippian Barnette Shale of Texas and the Caney Shale of southern Oklahoma: Oklahoma Geologic Survey, Open File Report 6-2006, 89 p.

4. Paleoclimate and the origin of Paleozoic chert: time to re-examine the origins of chert in the rock record;Cecil,;The Sedimentary Record,2015

5. The chemistry of eolian quartz dust and the origin of chert;Cecil,;Journal of Sedimentary Research,2018