Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/68123
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dc.contributor.authorPatcharin Kosuwan Jundeeen_US
dc.contributor.authorBurapha Phajuyen_US
dc.contributor.authorYuenyong Panjasawatwongen_US
dc.date.accessioned2020-04-02T15:21:03Z-
dc.date.available2020-04-02T15:21:03Z-
dc.date.issued2019-11-01en_US
dc.identifier.issn01253395en_US
dc.identifier.other2-s2.0-85075449199en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85075449199&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/68123-
dc.description.abstract© 2019, Prince of Songkla University. All rights reserved. The volcanic rocks of the Chae Hom area in Lampang, northern Thailand were investigated. Petrographic and geochemical analyses were performed to comprehend the alterations. The volcanic rocks in this study were co-magmatic and chemically transitional rhyolite to trachyandesite with calc-alkalic affinity. Their colors were highly variable due to two main alteration processes that included silicification and sericitization. The silicification process yields abundant quartz, whereas the sericitization yields abundant sericite and clay minerals. The sericite and clay minerals are most likely to be illite. The silica-fication process occurred after the sericitization process. Based on our petrochemical analysis, the Chae Hom volcanic rocks are considered to be of calc-alkaline affinity and post-collisional magmatic suite.en_US
dc.subjectMultidisciplinaryen_US
dc.titleSericitization-silicification of chae hom volcanics at lampang in Northern Thailanden_US
dc.typeJournalen_US
article.title.sourcetitleSongklanakarin Journal of Science and Technologyen_US
article.volume41en_US
article.stream.affiliationsChiang Mai Universityen_US
Appears in Collections:CMUL: Journal Articles

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