Are basal Ediacaran (635 Ma) post-glacial "cap dolostones" diachronous?

dc.contributor.authorHoffman, P.
dc.contributor.authorHalverson, G.
dc.contributor.authorDomack, E.
dc.contributor.authorHusson, J.
dc.contributor.authorHiggins, J.
dc.contributor.authorSchrag, D.
dc.date.issued2007
dc.descriptionCopyright © 2007 Elsevier B.V. All rights reserved.
dc.description.statementofresponsibilityPaul F. Hoffman, Galen P. Halverson, Eugene W. Domack, Jonathan M. Husson, John A. Higgins and Daniel P. Schrag
dc.description.urihttp://www.elsevier.com/wps/find/journaldescription.cws_home/503328/description#description
dc.identifier.citationEarth and Planetary Science Letters, 2007; 258(1-2):114-131
dc.identifier.doi10.1016/j.epsl.2007.03.032
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/2440/43893
dc.language.isoen
dc.publisherElsevier Science BV
dc.source.urihttps://doi.org/10.1016/j.epsl.2007.03.032
dc.titleAre basal Ediacaran (635 Ma) post-glacial "cap dolostones" diachronous?
dc.typeJournal article
pubs.publication-statusPublished

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