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Hagadorn, James W., Bottjer, David J. (1997) Wrinkle structures: Microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition. Geology, 25 (11) 1047 doi:10.1130/0091-7613(1997)025<1047:wsmmss>2.3.co;2

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Reference TypeJournal (article/letter/editorial)
TitleWrinkle structures: Microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition
JournalGeology
AuthorsHagadorn, James W.Author
Bottjer, David J.Author
Year1997Volume25
Issue11
PublisherGeological Society of America
DOIdoi:10.1130/0091-7613(1997)025<1047:wsmmss>2.3.co;2Search in ResearchGate
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Mindat Ref. ID136475Long-form Identifiermindat:1:5:136475:4
GUID0
Full ReferenceHagadorn, James W., Bottjer, David J. (1997) Wrinkle structures: Microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition. Geology, 25 (11) 1047 doi:10.1130/0091-7613(1997)025<1047:wsmmss>2.3.co;2
Plain TextHagadorn, James W., Bottjer, David J. (1997) Wrinkle structures: Microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition. Geology, 25 (11) 1047 doi:10.1130/0091-7613(1997)0252.3.co;2
In(1997) Geology Vol. 25 (11) Geological Society of America

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Schubert, Jennifer K., Kidder, David L., Erwin, Douglas H. (1997) Silica-replaced fossils through the Phanerozoic. Geology, 25 (11) 1031 doi:10.1130/0091-7613(1997)025<1031:srfttp>2.3.co;2
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