Wenhong Qiu (Johnson)\n\u90b1\u6587\u6d2a<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tPOST-DOCTORAL RESEARCHER<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t\t\t\t\t\t\t![\"\"](\"https:\/\/ise.usj.edu.mo\/wp-content\/uploads\/2019\/02\/\u90b1\u6587\u6d2a\uff0cQiu-Wenhong-Johnson-photo_small.jpg\")
\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Research Gate: <\/span>Qiu\u00a0Wenhong<\/a><\/li>
- ORCID ID:<\/li>
- SCOPUS ID:<\/li><\/ul>
E-mail: johnson.qiu@usj.edu.mo ; qiuwenhong1990@qq.com<\/p>
EDUCATION:\u00a0<\/strong>2013 BSc in Geology, School of Earth Science and Engineering, Nanjing University;\u00a0<\/span>2018 PhD in Petrology and Geochemistry, Department of Earth Sciences, The University of Hong Kong<\/span><\/p>ACADEMIC PROFESSIONAL EXPERIENCE:\u00a0<\/strong>2018 to 2019 Feb, Research Assistant, The University of Hong Kong;\u00a0<\/span>since 2019, Postdoctoral position, University of Saint Joseph<\/span><\/p><\/div><\/div>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tRESEARCH INTERESTS<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\tMy research focuses on (1) Paleozoic sedimentary exhalative sulfide (SEDEX) deposits, volcanic hosted massive sulfide (VHMS) deposits and Mississippi Valley-type sulfide (MVT) deposits in South China, and (2) seafloor massive sulfide deposits (SMS) formed in hydrothermal systems from slower spreading mid-ocean ridges, like the Mid-Atlantic Ridge and the Southwest Indian Ridge.<\/span><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tSELECTED RESEARCH PROJECTS<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\tSWIMAR<\/a>\u00a0\u2013\u00a0The role of ultramafic-hosted hydrothermal systems in the formation of seafloor deposits: comparison between SWIR and MAR fields\/\u8d85\u57fa\u6027\u5ca9\u7cfb\u6d77\u5e95\u71b1\u6cc9\u7cfb\u7d71\u65bc\u6d77\u5e8a\u71b1\u6db2\u7926\u5e8a\u626e\u6f14\u4e4b\u89d2\u8272:\u4ee5\u00a0SWIR\u00a0\u53ca\u00a0MAR\u00a0\u71b1\u6cc9\u7cfb\u7d71\u76f8\u4e92\u6bd4\u8f03\u70ba\u4f8b<\/a>. FDCT File No.: 002\/2018\/A1, 2018-2021 (team member)<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tSELECTED PUBLICATIONS<\/h4>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Wu, Q., Zhao, T. P., Chen, W. T., Gao, X. Y., Meng, L., & Qiu, W.\u00a0(2021). Origin of the Qiyugou gold deposit in the southern margin of the North China Craton: Insights from trace elements of pyrite and mineralogy of Bi-minerals. Ore Geology Reviews, 104085.Qiu, W. J., Zhou, M.-F., Li, X., Huang, F., Malpas, (2021) Constraints of Fe-S-C stable isotopes on hydrothermal and microbial activities during formation of sediment-hosted stratiform sulfide deposits. Geochimica et Cosmochimica Acta. 313, 15. 195-213<\/li>
- Qiu, W.,\u00a0Zhou, M. F., Li, X., Williams-Jones, A. E., & Yuan, H. (2018). The Genesis of the Giant Dajiangping SEDEX-Type Pyrite Deposit, South China.\u00a0Economic Geology,\u00a0113(6), 1419-1446.<\/li>
- Qiu, W., Zhou, M. F., & Liu, Z. R. (2018). Late Paleozoic SEDEX deposits in South China formed in a carbonate platform at the northern margin of Gondwana.\u00a0Journal of Asian Earth Sciences,\u00a0156, 41-58.<\/li>
- Yuan, H., Liu, X., Chen, L., Bao, Z., Chen, K., Zong, C., … & Qiu, W., (2018). Simultaneous measurement of sulfur and lead isotopes in sulfides using nanosecond laser ablation coupled with two multi-collector inductively coupled plasma mass spectrometers. Journal of Asian Earth Sciences, 154, 386-396.<\/li>
- Li, G., Hartmann, J., Derry, L. A., West, A. J., You, C. F., Long, X., Zhan, T., Li, L., Li, G., Qiu, W., Li, T., Liu, L., Chen, Y., Ji, J., Zhao, L., Chen, J. (2016). Temperature dependence of basalt weathering.\u00a0Earth and Planetary Science Letters,\u00a0443, 59-69.<\/li>
- Chen, W., Xu, Z., Qiu, W., Li, C., Yu, Y., Wang, H., & Su, Y. (2015). Petrogenesis of the Yaochong granite and Mo deposit, Western Dabie orogen, eastern-central China: Constraints from zircon U\u2013Pb and molybdenite Re\u2013Os ages, whole-rock geochemistry and Sr\u2013Nd\u2013Pb\u2013Hf isotopes.\u00a0Journal of Asian Earth Sciences,\u00a0103, 198-211.<\/li><\/ul>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t
SELECTED COMMUNICATIONS<\/h4>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Qiu W<\/strong>, Dias \u00c1 A, Costa IMA & Barriga F (2022) The evolution of sulfur isotope in hydrothermal fluids along the formation of chimney of Menez Gwen (MAR): mineralization implications Goldschmidt2022<\/span><\/span><\/span><\/li>
- Qiu, W.<\/strong><\/span>, Dias, A. A., Costa, P. <\/span>(2020) Ore-Forming Process of the Menez Gwen Hydrothermal Field: In situ S Isotopes and Trace Metals Constraints. Poster presentation at the Goldschmidt Conference 2020 (online), Hawaii, USA.<\/span><\/li>
- Qiu, W.<\/strong>, Zhou, M. F., (2019, Oct) Interaction between hydrothermal and biological activities on a paleo-venting seafloor during formation of a SEDEX pyrite deposit. Oral presentation at the 2019 International Symposium on Low-temperature Mineralization, Guiyang, China.<\/span><\/li>
- Qiu, W.<\/strong>, Dias, A. A., Tao, C., Barriga, F. <\/span>(2019, Sep) Sulfide mineralization of the Saldanha hydrothermal field (MAR): constraints from the in-situ sulfur isotope microanalysis. Oral presentation at the InterRidge workshop on hydrothermal ore-forming process and the fate of SMS deposits along slow and ultraslow MOR, Hangzhou, China.<\/span><\/span><\/li>
- Qiu, W<\/strong>, Dias, \u00c1 A, Costa, P\u00a0<\/span>(2019, April) Hydrothermal fields at Mid-Atalantic Ridge, near Azores (Portugal). Poster presentation at The 17th Annual Conference of the Chinese Society of Mineralogy Petrology and Geochemistry, Hangzhou, China.<\/span><\/span><\/li>
- Qiu, W.<\/strong>, Zhou M. F. (2017, June). <\/span>Sulfur isotopic constraints on the origin of the Dajiangping SEDEX-type pyrite deposit, South China. Oral presentation at the FUTORES II Conference, Townsville, Australia.<\/span><\/span><\/li><\/ul>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"Wenhong Qiu (Johnson) \u90b1\u6587\u6d2a POST-DOCTORAL RESEARCHER Research Gate: Qiu\u00a0Wenhong ORCID ID: SCOPUS ID: E-mail: johnson.qiu@usj.edu.mo ; qiuwenhong1990@qq.com EDUCATION:\u00a02013 BSc in Geology, School of Earth Science and Engineering, Nanjing University;\u00a02018 PhD in Petrology and Geochemistry, Department of Earth Sciences, The University of Hong Kong ACADEMIC PROFESSIONAL EXPERIENCE:\u00a02018 to 2019 Feb, Research Assistant, The University of Hong […]<\/p>\n","protected":false},"author":4,"featured_media":0,"parent":454,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"elementor_header_footer","meta":{"protect_children":false,"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[],"tags":[],"class_list":["post-12838","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/comments?post=12838"}],"version-history":[{"count":45,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838\/revisions"}],"predecessor-version":[{"id":17767,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838\/revisions\/17767"}],"up":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/454"}],"wp:attachment":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/media?parent=12838"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/categories?post=12838"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/tags?post=12838"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
POST-DOCTORAL RESEARCHER<\/h2>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Research Gate: <\/span>Qiu\u00a0Wenhong<\/a><\/li>
- ORCID ID:<\/li>
- SCOPUS ID:<\/li><\/ul>
E-mail: johnson.qiu@usj.edu.mo ; qiuwenhong1990@qq.com<\/p>
EDUCATION:\u00a0<\/strong>2013 BSc in Geology, School of Earth Science and Engineering, Nanjing University;\u00a0<\/span>2018 PhD in Petrology and Geochemistry, Department of Earth Sciences, The University of Hong Kong<\/span><\/p>ACADEMIC PROFESSIONAL EXPERIENCE:\u00a0<\/strong>2018 to 2019 Feb, Research Assistant, The University of Hong Kong;\u00a0<\/span>since 2019, Postdoctoral position, University of Saint Joseph<\/span><\/p><\/div><\/div>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tRESEARCH INTERESTS<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\tMy research focuses on (1) Paleozoic sedimentary exhalative sulfide (SEDEX) deposits, volcanic hosted massive sulfide (VHMS) deposits and Mississippi Valley-type sulfide (MVT) deposits in South China, and (2) seafloor massive sulfide deposits (SMS) formed in hydrothermal systems from slower spreading mid-ocean ridges, like the Mid-Atlantic Ridge and the Southwest Indian Ridge.<\/span><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tSELECTED RESEARCH PROJECTS<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\tSWIMAR<\/a>\u00a0\u2013\u00a0The role of ultramafic-hosted hydrothermal systems in the formation of seafloor deposits: comparison between SWIR and MAR fields\/\u8d85\u57fa\u6027\u5ca9\u7cfb\u6d77\u5e95\u71b1\u6cc9\u7cfb\u7d71\u65bc\u6d77\u5e8a\u71b1\u6db2\u7926\u5e8a\u626e\u6f14\u4e4b\u89d2\u8272:\u4ee5\u00a0SWIR\u00a0\u53ca\u00a0MAR\u00a0\u71b1\u6cc9\u7cfb\u7d71\u76f8\u4e92\u6bd4\u8f03\u70ba\u4f8b<\/a>. FDCT File No.: 002\/2018\/A1, 2018-2021 (team member)<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tSELECTED PUBLICATIONS<\/h4>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Wu, Q., Zhao, T. P., Chen, W. T., Gao, X. Y., Meng, L., & Qiu, W.\u00a0(2021). Origin of the Qiyugou gold deposit in the southern margin of the North China Craton: Insights from trace elements of pyrite and mineralogy of Bi-minerals. Ore Geology Reviews, 104085.Qiu, W. J., Zhou, M.-F., Li, X., Huang, F., Malpas, (2021) Constraints of Fe-S-C stable isotopes on hydrothermal and microbial activities during formation of sediment-hosted stratiform sulfide deposits. Geochimica et Cosmochimica Acta. 313, 15. 195-213<\/li>
- Qiu, W.,\u00a0Zhou, M. F., Li, X., Williams-Jones, A. E., & Yuan, H. (2018). The Genesis of the Giant Dajiangping SEDEX-Type Pyrite Deposit, South China.\u00a0Economic Geology,\u00a0113(6), 1419-1446.<\/li>
- Qiu, W., Zhou, M. F., & Liu, Z. R. (2018). Late Paleozoic SEDEX deposits in South China formed in a carbonate platform at the northern margin of Gondwana.\u00a0Journal of Asian Earth Sciences,\u00a0156, 41-58.<\/li>
- Yuan, H., Liu, X., Chen, L., Bao, Z., Chen, K., Zong, C., … & Qiu, W., (2018). Simultaneous measurement of sulfur and lead isotopes in sulfides using nanosecond laser ablation coupled with two multi-collector inductively coupled plasma mass spectrometers. Journal of Asian Earth Sciences, 154, 386-396.<\/li>
- Li, G., Hartmann, J., Derry, L. A., West, A. J., You, C. F., Long, X., Zhan, T., Li, L., Li, G., Qiu, W., Li, T., Liu, L., Chen, Y., Ji, J., Zhao, L., Chen, J. (2016). Temperature dependence of basalt weathering.\u00a0Earth and Planetary Science Letters,\u00a0443, 59-69.<\/li>
- Chen, W., Xu, Z., Qiu, W., Li, C., Yu, Y., Wang, H., & Su, Y. (2015). Petrogenesis of the Yaochong granite and Mo deposit, Western Dabie orogen, eastern-central China: Constraints from zircon U\u2013Pb and molybdenite Re\u2013Os ages, whole-rock geochemistry and Sr\u2013Nd\u2013Pb\u2013Hf isotopes.\u00a0Journal of Asian Earth Sciences,\u00a0103, 198-211.<\/li><\/ul>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t
SELECTED COMMUNICATIONS<\/h4>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Qiu W<\/strong>, Dias \u00c1 A, Costa IMA & Barriga F (2022) The evolution of sulfur isotope in hydrothermal fluids along the formation of chimney of Menez Gwen (MAR): mineralization implications Goldschmidt2022<\/span><\/span><\/span><\/li>
- Qiu, W.<\/strong><\/span>, Dias, A. A., Costa, P. <\/span>(2020) Ore-Forming Process of the Menez Gwen Hydrothermal Field: In situ S Isotopes and Trace Metals Constraints. Poster presentation at the Goldschmidt Conference 2020 (online), Hawaii, USA.<\/span><\/li>
- Qiu, W.<\/strong>, Zhou, M. F., (2019, Oct) Interaction between hydrothermal and biological activities on a paleo-venting seafloor during formation of a SEDEX pyrite deposit. Oral presentation at the 2019 International Symposium on Low-temperature Mineralization, Guiyang, China.<\/span><\/li>
- Qiu, W.<\/strong>, Dias, A. A., Tao, C., Barriga, F. <\/span>(2019, Sep) Sulfide mineralization of the Saldanha hydrothermal field (MAR): constraints from the in-situ sulfur isotope microanalysis. Oral presentation at the InterRidge workshop on hydrothermal ore-forming process and the fate of SMS deposits along slow and ultraslow MOR, Hangzhou, China.<\/span><\/span><\/li>
- Qiu, W<\/strong>, Dias, \u00c1 A, Costa, P\u00a0<\/span>(2019, April) Hydrothermal fields at Mid-Atalantic Ridge, near Azores (Portugal). Poster presentation at The 17th Annual Conference of the Chinese Society of Mineralogy Petrology and Geochemistry, Hangzhou, China.<\/span><\/span><\/li>
- Qiu, W.<\/strong>, Zhou M. F. (2017, June). <\/span>Sulfur isotopic constraints on the origin of the Dajiangping SEDEX-type pyrite deposit, South China. Oral presentation at the FUTORES II Conference, Townsville, Australia.<\/span><\/span><\/li><\/ul>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"Wenhong Qiu (Johnson) \u90b1\u6587\u6d2a POST-DOCTORAL RESEARCHER Research Gate: Qiu\u00a0Wenhong ORCID ID: SCOPUS ID: E-mail: johnson.qiu@usj.edu.mo ; qiuwenhong1990@qq.com EDUCATION:\u00a02013 BSc in Geology, School of Earth Science and Engineering, Nanjing University;\u00a02018 PhD in Petrology and Geochemistry, Department of Earth Sciences, The University of Hong Kong ACADEMIC PROFESSIONAL EXPERIENCE:\u00a02018 to 2019 Feb, Research Assistant, The University of Hong […]<\/p>\n","protected":false},"author":4,"featured_media":0,"parent":454,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"elementor_header_footer","meta":{"protect_children":false,"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[],"tags":[],"class_list":["post-12838","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/comments?post=12838"}],"version-history":[{"count":45,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838\/revisions"}],"predecessor-version":[{"id":17767,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838\/revisions\/17767"}],"up":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/454"}],"wp:attachment":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/media?parent=12838"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/categories?post=12838"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/tags?post=12838"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t- Research Gate: <\/span>Qiu\u00a0Wenhong<\/a><\/li>
- ORCID ID:<\/li>
- SCOPUS ID:<\/li><\/ul>
E-mail: johnson.qiu@usj.edu.mo ; qiuwenhong1990@qq.com<\/p>
EDUCATION:\u00a0<\/strong>2013 BSc in Geology, School of Earth Science and Engineering, Nanjing University;\u00a0<\/span>2018 PhD in Petrology and Geochemistry, Department of Earth Sciences, The University of Hong Kong<\/span><\/p>
ACADEMIC PROFESSIONAL EXPERIENCE:\u00a0<\/strong>2018 to 2019 Feb, Research Assistant, The University of Hong Kong;\u00a0<\/span>since 2019, Postdoctoral position, University of Saint Joseph<\/span><\/p><\/div><\/div>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t \n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\n\t\t\t\t\t\t \n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tRESEARCH INTERESTS<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\tMy research focuses on (1) Paleozoic sedimentary exhalative sulfide (SEDEX) deposits, volcanic hosted massive sulfide (VHMS) deposits and Mississippi Valley-type sulfide (MVT) deposits in South China, and (2) seafloor massive sulfide deposits (SMS) formed in hydrothermal systems from slower spreading mid-ocean ridges, like the Mid-Atlantic Ridge and the Southwest Indian Ridge.<\/span><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t
\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tSELECTED RESEARCH PROJECTS<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\tSWIMAR<\/a>\u00a0\u2013\u00a0The role of ultramafic-hosted hydrothermal systems in the formation of seafloor deposits: comparison between SWIR and MAR fields\/\u8d85\u57fa\u6027\u5ca9\u7cfb\u6d77\u5e95\u71b1\u6cc9\u7cfb\u7d71\u65bc\u6d77\u5e8a\u71b1\u6db2\u7926\u5e8a\u626e\u6f14\u4e4b\u89d2\u8272:\u4ee5\u00a0SWIR\u00a0\u53ca\u00a0MAR\u00a0\u71b1\u6cc9\u7cfb\u7d71\u76f8\u4e92\u6bd4\u8f03\u70ba\u4f8b<\/a>. FDCT File No.: 002\/2018\/A1, 2018-2021 (team member)<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t \n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\tSELECTED PUBLICATIONS<\/h4>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Wu, Q., Zhao, T. P., Chen, W. T., Gao, X. Y., Meng, L., & Qiu, W.\u00a0(2021). Origin of the Qiyugou gold deposit in the southern margin of the North China Craton: Insights from trace elements of pyrite and mineralogy of Bi-minerals. Ore Geology Reviews, 104085.Qiu, W. J., Zhou, M.-F., Li, X., Huang, F., Malpas, (2021) Constraints of Fe-S-C stable isotopes on hydrothermal and microbial activities during formation of sediment-hosted stratiform sulfide deposits. Geochimica et Cosmochimica Acta. 313, 15. 195-213<\/li>
- Qiu, W.,\u00a0Zhou, M. F., Li, X., Williams-Jones, A. E., & Yuan, H. (2018). The Genesis of the Giant Dajiangping SEDEX-Type Pyrite Deposit, South China.\u00a0Economic Geology,\u00a0113(6), 1419-1446.<\/li>
- Qiu, W., Zhou, M. F., & Liu, Z. R. (2018). Late Paleozoic SEDEX deposits in South China formed in a carbonate platform at the northern margin of Gondwana.\u00a0Journal of Asian Earth Sciences,\u00a0156, 41-58.<\/li>
- Yuan, H., Liu, X., Chen, L., Bao, Z., Chen, K., Zong, C., … & Qiu, W., (2018). Simultaneous measurement of sulfur and lead isotopes in sulfides using nanosecond laser ablation coupled with two multi-collector inductively coupled plasma mass spectrometers. Journal of Asian Earth Sciences, 154, 386-396.<\/li>
- Li, G., Hartmann, J., Derry, L. A., West, A. J., You, C. F., Long, X., Zhan, T., Li, L., Li, G., Qiu, W., Li, T., Liu, L., Chen, Y., Ji, J., Zhao, L., Chen, J. (2016). Temperature dependence of basalt weathering.\u00a0Earth and Planetary Science Letters,\u00a0443, 59-69.<\/li>
- Chen, W., Xu, Z., Qiu, W., Li, C., Yu, Y., Wang, H., & Su, Y. (2015). Petrogenesis of the Yaochong granite and Mo deposit, Western Dabie orogen, eastern-central China: Constraints from zircon U\u2013Pb and molybdenite Re\u2013Os ages, whole-rock geochemistry and Sr\u2013Nd\u2013Pb\u2013Hf isotopes.\u00a0Journal of Asian Earth Sciences,\u00a0103, 198-211.<\/li><\/ul>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t
SELECTED COMMUNICATIONS<\/h4>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\t\t- Qiu W<\/strong>, Dias \u00c1 A, Costa IMA & Barriga F (2022) The evolution of sulfur isotope in hydrothermal fluids along the formation of chimney of Menez Gwen (MAR): mineralization implications Goldschmidt2022<\/span><\/span><\/span><\/li>
- Qiu, W.<\/strong><\/span>, Dias, A. A., Costa, P. <\/span>(2020) Ore-Forming Process of the Menez Gwen Hydrothermal Field: In situ S Isotopes and Trace Metals Constraints. Poster presentation at the Goldschmidt Conference 2020 (online), Hawaii, USA.<\/span><\/li>
- Qiu, W.<\/strong>, Zhou, M. F., (2019, Oct) Interaction between hydrothermal and biological activities on a paleo-venting seafloor during formation of a SEDEX pyrite deposit. Oral presentation at the 2019 International Symposium on Low-temperature Mineralization, Guiyang, China.<\/span><\/li>
- Qiu, W.<\/strong>, Dias, A. A., Tao, C., Barriga, F. <\/span>(2019, Sep) Sulfide mineralization of the Saldanha hydrothermal field (MAR): constraints from the in-situ sulfur isotope microanalysis. Oral presentation at the InterRidge workshop on hydrothermal ore-forming process and the fate of SMS deposits along slow and ultraslow MOR, Hangzhou, China.<\/span><\/span><\/li>
- Qiu, W<\/strong>, Dias, \u00c1 A, Costa, P\u00a0<\/span>(2019, April) Hydrothermal fields at Mid-Atalantic Ridge, near Azores (Portugal). Poster presentation at The 17th Annual Conference of the Chinese Society of Mineralogy Petrology and Geochemistry, Hangzhou, China.<\/span><\/span><\/li>
- Qiu, W.<\/strong>, Zhou M. F. (2017, June). <\/span>Sulfur isotopic constraints on the origin of the Dajiangping SEDEX-type pyrite deposit, South China. Oral presentation at the FUTORES II Conference, Townsville, Australia.<\/span><\/span><\/li><\/ul>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t \n\t\t\t\t\t\n\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\n\t\t\t\t\t\n\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"Wenhong Qiu (Johnson) \u90b1\u6587\u6d2a POST-DOCTORAL RESEARCHER Research Gate: Qiu\u00a0Wenhong ORCID ID: SCOPUS ID: E-mail: johnson.qiu@usj.edu.mo ; qiuwenhong1990@qq.com EDUCATION:\u00a02013 BSc in Geology, School of Earth Science and Engineering, Nanjing University;\u00a02018 PhD in Petrology and Geochemistry, Department of Earth Sciences, The University of Hong Kong ACADEMIC PROFESSIONAL EXPERIENCE:\u00a02018 to 2019 Feb, Research Assistant, The University of Hong […]<\/p>\n","protected":false},"author":4,"featured_media":0,"parent":454,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"elementor_header_footer","meta":{"protect_children":false,"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[],"tags":[],"class_list":["post-12838","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/comments?post=12838"}],"version-history":[{"count":45,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838\/revisions"}],"predecessor-version":[{"id":17767,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/12838\/revisions\/17767"}],"up":[{"embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/pages\/454"}],"wp:attachment":[{"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/media?parent=12838"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/categories?post=12838"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ise.usj.edu.mo\/wp-json\/wp\/v2\/tags?post=12838"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
- Qiu, W.<\/strong><\/span>, Dias, A. A., Costa, P. <\/span>(2020) Ore-Forming Process of the Menez Gwen Hydrothermal Field: In situ S Isotopes and Trace Metals Constraints. Poster presentation at the Goldschmidt Conference 2020 (online), Hawaii, USA.<\/span><\/li>
- Qiu W<\/strong>, Dias \u00c1 A, Costa IMA & Barriga F (2022) The evolution of sulfur isotope in hydrothermal fluids along the formation of chimney of Menez Gwen (MAR): mineralization implications Goldschmidt2022<\/span><\/span><\/span><\/li>