{"id":35017,"date":"2024-12-09T11:56:08","date_gmt":"2024-12-09T03:56:08","guid":{"rendered":"https:\/\/www.oc.ntu.edu.tw\/?p=35017"},"modified":"2024-12-09T11:58:19","modified_gmt":"2024-12-09T03:58:19","slug":"decoding-climate-signals-and-non-climate-variability-in-paleotemperature-records","status":"publish","type":"post","link":"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35017\/","title":{"rendered":"Unveiling attenuation structures in the northern Taiwan volcanic zone"},"content":{"rendered":"\n<p>Situated at the dynamic convergent boundary between the Philippine Sea Plate and the Eurasian Plate, Taiwan experiences moderate earthquakes and notable volcanic activity, particularly in the Tatun Volcanic Group.<\/p>\n\n\n\n<p>Assistant Professor Justin Yen-Ting Ko and his research team investigate regional magmatism in northern Taiwan using advanced three-dimensional, frequency-dependent attenuation tomography of P- and S-waves. Employing high-resolution data from the Formosa seismic array, they identify high-attenuation anomalies (low Q) beneath the Northern Taiwan Volcanic Zone (NTVZ) and offshore submarine volcanoes, indicative of potential hydrothermal activities and magma reservoirs at varying depths. Additionally, they observe low-attenuation anomalies (high Q) in the forearc region of the Ryukyu subduction zone, suggesting partial saturation linked to serpentinization processes resulting from seawater infiltration or forearc mantle hydration.<\/p>\n\n\n\n<p>These findings illuminate complex geological features and provide essential insights into the crustal properties of northern Taiwan, contributing to a deeper understanding of its magmatic evolution and tectonic processes.<\/p>\n\n\n\n<p>The research was published in the Nature Research journal Scientific Reports:<br>Lin, Y.-P., Ko, J. Y.-T.*, Huang, B.-S., Lin, C.-H., and Shih, M.-H. (2024). Unveiling attenuation structures in the northern Taiwan volcanic zone. Sci Rep 14, 4716. <a href=\"https:\/\/doi.org\/10.1038\/s41598-024-55397-8\">https:\/\/doi.org\/10.1038\/s41598-024-55397-8<\/a><\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img fetchpriority=\"high\" decoding=\"async\" width=\"660\" height=\"721\" src=\"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2024\/12\/\u87a2\u5e55\u64f7\u53d6\u756b\u9762-2024-12-09-115233.png\" alt=\"\" class=\"wp-image-35023\"\/><\/figure>\n\n\n\n<p>Fig. 1. Cross-sections of \u0394lnQP(x,f0) (left side) and \u0394lnQS(x,f0) (right side) through the northern Taiwan attenuation tomography model. Red triangles indicate the locations of volcanoes.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Situated at the dynamic convergent boundary between the Philippine Sea Plate and the Eurasian Plate, Taiwan experiences moderate earthquakes and notable volcanic activity, particularly in the Tatun Volcanic Group. Assistant Professor Justin Yen-Ting Ko and his research team investigate regional magmatism in northern Taiwan using advanced three-dimensional, frequency-dependent attenuation tomography of P- and S-waves. Employing [&hellip;]<\/p>\n","protected":false},"author":16,"featured_media":35023,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[95,119],"tags":[],"class_list":["post-35017","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-news-en","category-research-highlights"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.3 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Unveiling attenuation structures in the northern Taiwan volcanic zone - Institute of Oceanography, NTU<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35017\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Unveiling attenuation structures in the northern Taiwan volcanic zone - Institute of Oceanography, NTU\" \/>\n<meta property=\"og:description\" content=\"Situated at the dynamic convergent boundary between the Philippine Sea Plate and the Eurasian Plate, Taiwan experiences moderate earthquakes and notable volcanic activity, particularly in the Tatun Volcanic Group. Assistant Professor Justin Yen-Ting Ko and his research team investigate regional magmatism in northern Taiwan using advanced three-dimensional, frequency-dependent attenuation tomography of P- and S-waves. Employing [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35017\/\" \/>\n<meta property=\"og:site_name\" content=\"Institute of Oceanography, NTU\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/IONTUTW\" \/>\n<meta property=\"article:published_time\" content=\"2024-12-09T03:56:08+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2024-12-09T03:58:19+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2024\/12\/\u87a2\u5e55\u64f7\u53d6\u756b\u9762-2024-12-09-115233.png\" \/>\n\t<meta property=\"og:image:width\" content=\"660\" \/>\n\t<meta property=\"og:image:height\" content=\"721\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/png\" \/>\n<meta name=\"author\" content=\"\u660e\u8b19\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta 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