Articles | Volume 9, issue 6
Research article
21 Dec 2018
Research article |  | 21 Dec 2018

From widespread Mississippian to localized Pennsylvanian extension in central Spitsbergen, Svalbard

Jean-Baptiste P. Koehl and Jhon M. Muñoz-Barrera


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Jean-Baptiste Koehl on behalf of the Authors (27 Nov 2018)  Author's response    Manuscript
ED: Publish as is (07 Dec 2018) by Mark Allen
ED: Publish as is (07 Dec 2018) by Federico Rossetti(Executive Editor)
Short summary
This research is dedicated to the study of poorly understood coal-bearing Mississippian (ca. 360–325 Ma) sedimentary rocks in central Spitsbergen. Our results suggest that these rocks were deposited during a period of widespread extension involving multiple fault trends, including faults striking subparallel to the extension direction, while overlying Pennsylvanian rocks (ca. 325–300 Ma) were deposited during extension localized along fewer, larger faults.