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dc.contributor.authorPatcharin Kosuwan Jundeeen_US
dc.contributor.authorPhisit Limtrakunen_US
dc.contributor.authorApichet Boonsoongen_US
dc.contributor.authorYuenyong Panjasawatwongen_US
dc.date.accessioned2019-05-07T09:59:42Z-
dc.date.available2019-05-07T09:59:42Z-
dc.date.issued2017en_US
dc.identifier.issn0125-2526en_US
dc.identifier.urihttp://it.science.cmu.ac.th/ejournal/dl.php?journal_id=8498en_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/63990-
dc.description.abstractThe felsic to mafic volcanic/hypabyssal rocks in the area of Nakhon Sawan and Uthai Thani Provinces, Upper Central Plain Thailand were distributed in the area of Tha Tako, Krok Phra and Chum Ta Bong, covering an area of approximately 200 km2. The least-altered mafic to felsic volcanic/hypabyssal rock samples can be divided into five groups Group I rocks (calc-alkalic), Group II rocks (calc-alkalic), Group III rocks (tholeiitic), Group IV rocks (tholeiitic) and Group V rocks (shoshonitic) using REE patterns and N-MORB normalized multi-elements patterns. Group I rocks compose of rhyodacite/dacite, andesite/basalt and diorite/gabbro. Group II rocks compose of diorite/gabbro. Group III and Group IV rocks compose of andesite/basalt and microdiorite/microgabbro. Group V rocks compose of rhyodacite/dacite. N-MORB normalized multi-element patterns suggest that Groups I, II and V rocks have characteristics of subduction-related magma and Groups III and IV rocks have been crystallized from MORB-like magma that contains crustal signature.en_US
dc.languageEngen_US
dc.publisherScience Faculty of Chiang Mai Universityen_US
dc.titlePetrography and REE Geochemical Characteristics of Felsic to Mafic Volcanic /Hypabyssal Rock in Nakhon Sawan and Uthai Thani Provinces, Central Thailanden_US
dc.typeบทความวารสารen_US
article.title.sourcetitleChiang Mai Journal of Scienceen_US
article.volume44en_US
article.stream.affiliationsDepartment of Geological Sciences, Faculty of Science, Chiang Mai University, Chiang Mai 50200, Thailand.en_US
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