Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/1647
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dc.contributor.authorMetcalfe, Ianen
dc.date.accessioned2009-05-21T10:15:00Z
dc.date.issued2002en
dc.identifier.citationJournal of Asian Earth Sciences, 20(6), p. 551-566en
dc.identifier.issn1367-9120en
dc.identifier.urihttps://hdl.handle.net/1959.11/1647en
dc.description.abstractThe principal continental lithospheric terranes, now comprising SE Asia and that existed in the Permian, are the South China/Indochina Super Terrane, and the Sibumasu, Simao, West Burma and SW Borneo/Semitau terranes. The Simao Terrane is here regarded a separate terrane, derived from South China by back-arc spreading in the Lower Carboniferous, rather than as an extension of Indochina. The main Palaeo-Tethys ocean in Thailand is identified as being represented by the Chiang Mai and Sra Kaeo sutures, and the eastern boundary of the Sibumasu Terrane is thus interpreted to lie farther west in Thailand than previously inferred. The Nan-Uttaradit Suture is interpreted as representing a marginal back-arc basin, and contiguous with the Ailaoshan and Jinshajiang sutures in SW China. The South China/Indochina Super Terrane, and the Simao Terrane were located within the Palaeo-Tethys in equatorial latitudes during the Permian, where they, together with North China, exhibit Cathaysian floras and faunas. The Sibumasu Terrane was located on the NW Australian margin of Gondwana until the Sakmarian. Major shifts in faunal affinities from Gondwana province faunas to an independent Sibumasu Province and then to assimilation into the Cathaysian Province, records the separation and rapid northward drift of Sibumasu after the Late Sakmarian. The principal Permian palaeogeographic models for the region are assessed for internal consistencies and conflicts.en
dc.languageenen
dc.publisherPergamonen
dc.relation.ispartofJournal of Asian Earth Sciencesen
dc.titlePermian tectonic framework and palaeogeography of SE Asiaen
dc.typeJournal Articleen
dc.identifier.doi10.1016/S1367-9120(02)00022-6en
dc.subject.keywordsTectonicsen
local.contributor.firstnameIanen
local.subject.for2008040313 Tectonicsen
local.subject.seo770101 Climate changeen
local.profile.schoolSchool of Environmental and Rural Scienceen
local.profile.emailimetcal2@une.edu.auen
local.output.categoryC1en
local.record.placeauen
local.record.institutionUniversity of New Englanden
local.identifier.epublicationsrecordpes:166en
local.publisher.placeOxford, United Kingdomen
local.format.startpage551en
local.format.endpage566en
local.peerreviewedYesen
local.identifier.volume20en
local.identifier.issue6en
local.contributor.lastnameMetcalfeen
dc.identifier.staffune-id:imetcal2en
local.profile.roleauthoren
local.identifier.unepublicationidune:1706en
dc.identifier.academiclevelAcademicen
local.title.maintitlePermian tectonic framework and palaeogeography of SE Asiaen
local.output.categorydescriptionC1 Refereed Article in a Scholarly Journalen
local.description.statisticsepubsVisitors: 137<br />Views: 144<br />Downloads: 0en
local.search.authorMetcalfe, Ianen
local.uneassociationUnknownen
local.year.published2002en
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