Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/73248
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dc.contributor.authorBadr, M.en
dc.contributor.authorMasoudi, F.en
dc.contributor.authorCollins, A.en
dc.contributor.authorSorbi, A.en
dc.date.issued2012en
dc.identifier.citationActa Geologica Sinica-English Edition, 2012; 86(1):48-64en
dc.identifier.issn1000-9515en
dc.identifier.issn1755-6724en
dc.identifier.urihttp://hdl.handle.net/2440/73248-
dc.description.abstractThe Soursat metamorphic complex (SMC) in northwestern Iran is part of the Sanandaj–Sirjan metamorphic belt. The complex is composed of different metamorphic and plutonic rocks, but is dominated by metapelites composed of garnet, staurolite, kyanite, fibrolite, cordierite, and andalusite. Porphyroblasts in schists have the same fabric, and three stages of schistosity are present. The internal schistosity (Sn) inclusion trails are also offset by conjugate sets of extensional schistosity (Sn+1) and a second (Sn+2) that crenulates (Sn+1). Polyphase metamorphisms are present in the complex. Garnet, staurolite, kyanite, and fibrolite assemblage preserves conditions during the M1 metamorphic event. This assemblage yields a P–t estimate of 645±11°C and 6.5±0.5 kbar. Other samples of the central part of SMC contain cordierite and andalusite (M2) overgrowth that yields a P–t estimate of 532±33°C and 2.1±1.1 kbar.en
dc.description.statementofresponsibilityMahboobeh Jamshidi Badr, Fariborz Masoudi, Alan S. Collins and Ali Sorbien
dc.language.isoenen
dc.publisherGeological Soc Chinaen
dc.rights© 2012 Geological Society of Chinaen
dc.subjectmetamorphism; north-west Iran; Sanandaj-Sirjan zone; Soursat metamorphic complex.en
dc.titleMineralogical evidence for regional metamorphism overprinted by contact metamorphismen
dc.typeJournal articleen
dc.identifier.doi10.1111/j.1755-6724.2012.00610.xen
pubs.publication-statusPublisheden
dc.identifier.orcidCollins, A. [0000-0002-3408-5474]en
Appears in Collections:Geology & Geophysics publications

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