{"id":223,"date":"2025-12-24T18:10:26","date_gmt":"2025-12-24T09:10:26","guid":{"rendered":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/?p=223"},"modified":"2025-12-24T18:14:21","modified_gmt":"2025-12-24T09:14:21","slug":"a-paper-on-the-formation-of-li-pegmatite-has-been-published","status":"publish","type":"post","link":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/2025\/12\/24\/a-paper-on-the-formation-of-li-pegmatite-has-been-published\/","title":{"rendered":"A paper on the formation of Li-pegmatite has been published."},"content":{"rendered":"\n<p>In southern Thailand, a large lithium (Li) pegmatite deposit has been discovered. In this paper, we conclude that the formation of these granites and Li-pegmatites in the region is linked to orogenic events and plate subduction during the Late Triassic, Late Cretaceous, and Paleocene. The Li-pegmatites originated from highly fractionated tourmaline granite magma during the Late Cretaceous. This study was conducted as part of Dolnapha Phrairoj\u2019s master\u2019s research. <br><strong>Dolnapha Phrairoj,<\/strong> <strong>Mayuko Fukuyama,<\/strong> Ladda Tangwattananukul (2025) Geochemical and geochronological Constraints on the Petrogenesis and Tectonic Evolution of Li\u2010Pegmatites and Granites in Phang Nga and Phuket, Southern Thailand. Resource Geology, 76, e70024. (20 pages)<br><a href=\"https:\/\/onlinelibrary.wiley.com\/doi\/full\/10.1111\/rge.70024\" data-type=\"link\" data-id=\"https:\/\/onlinelibrary.wiley.com\/doi\/full\/10.1111\/rge.70024\" target=\"_blank\" rel=\"noreferrer noopener\">DOI: https:\/\/doi.org\/10.1111\/rge.70024<\/a><\/p>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>In southern Thailand, a large lithium (Li) pegmatite deposit has been discovered. In this paper, we conclude that the formation of these granites and Li-pegmatites in the region is linked to orogenic events and plate subduction during the Late Triassic, Late Cretaceous, and Paleocene. The Li-pegmatites originated from highly fractionated tourmaline granite magma during the [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5],"tags":[],"class_list":["post-223","post","type-post","status-publish","format-standard","hentry","category-publication"],"_links":{"self":[{"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/posts\/223","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/comments?post=223"}],"version-history":[{"count":6,"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/posts\/223\/revisions"}],"predecessor-version":[{"id":229,"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/posts\/223\/revisions\/229"}],"wp:attachment":[{"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/media?parent=223"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/categories?post=223"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.math.akita-u.ac.jp\/fukuyama\/en\/wp-json\/wp\/v2\/tags?post=223"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}