Diagenesis of spiculites and carbonates in a Permian temperate ramp succession - Tempelfjorden Group, Spitsbergen, Arctic Norway-Reference-Cited by-同舟云学术

Diagenesis of spiculites and carbonates in a Permian temperate ramp succession - Tempelfjorden Group, Spitsbergen, Arctic Norway

Published:2017-10-21 Issue:3 Volume:65 Page:745-774
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Matysik Michał¹,Stemmerik Lars¹²,Olaussen Snorre²,Brunstad Harald³

Affiliation:

1. Natural History Museum; University of Copenhagen; Øster Voldgade 5-7 DK-1350 Copenhagen K Denmark

2. The University Centre in Svalbard (UNIS); P.O. Box 156 N-9171 Longyearbyen Norway

3. Lundin Norway AS; Strandveien 4 P.O. Box 247 N-1326 Lysaker Norway

Funder

Lundin Norway AS through a grant to UNIS

Vetenskapsrådet

University of Iceland and a consortium of Danish geoscience institutions

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12404/fullpdf

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4. Facies analysis and depositional environments of a storm-dominated, temperate to cold, mixed siliceous-carbonate ramp: the Permian Kapp Starostin Formation in NE Svalbard;Blomeier;Norw. J. Geol.,2013

5. Structural outline of a Tertiary Basement-cored uplift/inversion structure in western Spitsbergen, Svalbard: kinematics and controlling factors;Braathen;Tectonics,1995

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