Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/105422
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dc.contributor.authorWang, J.en
dc.contributor.authorLi, S.en
dc.contributor.authorSantosh, M.en
dc.contributor.authorDai, L.en
dc.contributor.authorSuo, Y.en
dc.contributor.authorYu, S.en
dc.contributor.authorZhao, S.en
dc.contributor.authorLiu, B.en
dc.contributor.authorWang, Q.en
dc.date.issued2013en
dc.identifier.citationGeological Journal, 2013; 48(5):561-578en
dc.identifier.issn0072-1050en
dc.identifier.issn1099-1034en
dc.identifier.urihttp://hdl.handle.net/2440/105422-
dc.description.abstractAbstract not availableen
dc.description.statementofresponsibilityJ. D. Wang, S.Z.Li, M. Santosh, L. M. Dai, Y. H. Suo, S.Yu, S. J. Zhao, B. Liu, Q. J. Wangen
dc.language.isoenen
dc.publisherWiley-Blackwellen
dc.rightsCopyright © 2013 John Wiley & Sons, Ltd.en
dc.subjectDongying Sag; Bohai Bay Basin; lacustrine basin; Eocene turbidite sandstones; sedimentary model; seismic interpretation; North China Cratonen
dc.titleLacustrine turbidites in the Eocene Shahejie Formation, Dongying Sag, Bohai Bay Basin, North China Cratonen
dc.typeJournal articleen
dc.identifier.rmid0030044502en
dc.identifier.doi10.1002/gj.2517en
dc.identifier.pubid235363-
pubs.library.collectionGeology & Geophysics publicationsen
pubs.library.teamDS10en
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]en
Appears in Collections:Geology & Geophysics publications

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