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Article: Radiolarian age constraints on Mesotethyan ocean evolution, and their implications for development of the Bangong-Nujiang suture, Tibet

TitleRadiolarian age constraints on Mesotethyan ocean evolution, and their implications for development of the Bangong-Nujiang suture, Tibet
Authors
Baxter, ATAitchison, JCZyabrev, SV
Issue Date2009
PublisherGeological Society Publishing House. The Journal's web site is located at http://www.geolsoc.org.uk/gsl/publications/journals/jgs
Citation
Journal Of The Geological Society, 2009, v. 166 n. 4, p. 689-694 How to Cite?
DOI: http://dx.doi.org/10.1144/0016-76492008-128
AbstractRadiolarian discoveries indicate that deep-marine conditions prevailed in central Tibet from the early Middle Jurassic until well into the Early Cretaceous (late Hauterivian-early Aptian; 131-121 Ma) and help to constrain the temporal extent of oceanic conditions along the Bangong-Nujiang suture. These new fossils occur in chert or siliceous mudstone blocks associated with the Lagkor Tso ophiolitic mélange. Basin inversion associated with closure of Mesotethys between the Qiangtang and Lhasa terranes was accompanied by mélange formation and predated regionally widespread deposition of overlying shallow-marine late Aptian-Albian orbitolinid limestones. © 2009 Geological Society of London.
Persistent Identifierhttp://hdl.handle.net/10722/58650
ISSN
0016-7649
2023 Impact Factor: 2.6
2023 SCImago Journal Rankings: 1.166
ISI Accession Number ID
WOS:000267814700009
Funding AgencyGrant Number
Research Grant Council of Hong Kong Special Administrative Region, ChinaHKU7001/03
Funding Information:

We thank members of the Tibetan Geological Survey and the Tibetan Geological Society, whose efforts have helped to make this research possible, as have those Of Our colleagues in the HKUTRG. We thank P. Kapp, K. Zhang, E. Pessagno, I. Metcalfe and an anonymous reviewer for their constructive comments on versions of the manuscript. This research was supported by a grant from the Research Grant Council of Hong Kong Special Administrative Region, China (project HKU7001/03) awarded to J.C.A.

References
References in Scopus

 

DC FieldValueLanguage
dc.contributor.authorBaxter, ATen_HK
dc.contributor.authorAitchison, JCen_HK
dc.contributor.authorZyabrev, SVen_HK
dc.date.accessioned2010-05-31T03:34:23Z-
dc.date.available2010-05-31T03:34:23Z-
dc.date.issued2009en_HK
dc.identifier.citationJournal Of The Geological Society, 2009, v. 166 n. 4, p. 689-694en_HK
dc.identifier.issn0016-7649en_HK
dc.identifier.urihttp://hdl.handle.net/10722/58650-
dc.description.abstractRadiolarian discoveries indicate that deep-marine conditions prevailed in central Tibet from the early Middle Jurassic until well into the Early Cretaceous (late Hauterivian-early Aptian; 131-121 Ma) and help to constrain the temporal extent of oceanic conditions along the Bangong-Nujiang suture. These new fossils occur in chert or siliceous mudstone blocks associated with the Lagkor Tso ophiolitic mélange. Basin inversion associated with closure of Mesotethys between the Qiangtang and Lhasa terranes was accompanied by mélange formation and predated regionally widespread deposition of overlying shallow-marine late Aptian-Albian orbitolinid limestones. © 2009 Geological Society of London.en_HK
dc.languageengen_HK
dc.publisherGeological Society Publishing House. The Journal's web site is located at http://www.geolsoc.org.uk/gsl/publications/journals/jgsen_HK
dc.relation.ispartofJournal of the Geological Societyen_HK
dc.titleRadiolarian age constraints on Mesotethyan ocean evolution, and their implications for development of the Bangong-Nujiang suture, Tibeten_HK
dc.typeArticleen_HK
dc.identifier.emailAitchison, JC: jona@hku.hken_HK
dc.identifier.authorityAitchison, JC=rp00658en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1144/0016-76492008-128en_HK
dc.identifier.scopuseid_2-s2.0-69949119759en_HK
dc.identifier.hkuros162129en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-69949119759&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume166en_HK
dc.identifier.issue4en_HK
dc.identifier.spage689en_HK
dc.identifier.epage694en_HK
dc.identifier.isiWOS:000267814700009-
dc.publisher.placeUnited Kingdomen_HK
dc.identifier.scopusauthoridBaxter, AT=35069077600en_HK
dc.identifier.scopusauthoridAitchison, JC=7102533858en_HK
dc.identifier.scopusauthoridZyabrev, SV=6505935364en_HK
dc.identifier.issnl0016-7649-

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