*Morihisa Hamada1, Hikaru Iwamori1,2, Philipp A. Brandl3, Takayuki Ushikubo4, Kenji Shimizu4, Motoo Ito4, He Li5, Ivan P. Savov6 (1.Department of Solid Earth Geochemistry, Japan Agency for Marine-Earth Science and Technology, 2.Earthquake Research Institute, University of Tokyo, 3.GEOMAR Helmholtz Centre for Ocean Research Kiel, 4.Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology, 5.Institute of Oceanology, Chinese Academy of Sciences, 6.School of Earth and Environment, University of Leeds)
Session information
[E] Poster
S (Solid Earth Sciences ) » S-MP Mineralogy & Petrology
[S-MP30] Crust-Mantle Connections
Tue. May 28, 2019 10:45 AM - 12:15 PM Poster Hall (International Exhibition Hall8, Makuhari Messe)
convener:Yoshihiko Tamura(Research Institute for Marine Geodynamics, Japan Agency for Maine-Earth Science and Technology), Osamu Ishizuka(Geological Survey of Japan, AIST), Chris Conway(Geological Survey of Japan)
A paradigm of the solid Earth geochemical cycles is that the Earth's crust forms by melting of the Earth's upper peridotitic mantle. How divers is the spectrum of primary melts and which factors may contribute to its variations? What is the influence of crustal processing vs. primary magma diversity in creating the diversity of the Earth's crust? The session seeks to explore the crust-mantle connections at divergent and convergent plate boundaries, and oceanic island settings based on volcanology, petrology, geochemistry, geophysics, geochronology, and geodynamics studies.
*Hikaru Sawada1, Yukio Isozaki1, Shogo Aoki3, Shuhei Sakata2, Ryo Hasegawa1, Yasuo Nakamura1 (1.Department of General Systems Studies, the University of Tokyo, 2.Department of Chemistry, Gakushuin Universtiy, 3.Department of Applied Science, Okayama University of Science)
*Yasuhiro Hirai1, Yoshihiko Tamura2, Kaj Hoernle3, Christian Timm4, Folkmar Hauff3, Reinhard Werner3, Takeshi Hanyu2, Bogdan Vaglarov2, Qing Chang2, Takashi Miyazaki2, Jun-Ichi Kimura2 (1.Graduate School of Natural Science and Technology, Kanazawa University, Japan, 2.Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Kanagawa, Japan, 3.GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany, 4.GNS Science, Lower Hutt, New Zealand)
*Yoshihiko Tamura1, Tomoki Sato1, Osamu Ishizuka1,2, Takashi Miyazaki1, Yasuhiro Hirai1,3, Mami Takehara4, Eri Sakamoto5 (1.JAMSTEC, 2.AIST, 3.Kanazawa Univ., 4.NIPR, 5.NME)
*Yoshihiko Tamura1, Kentaro Kaneda2, Gou Fujie1, Akane Ohira1, Eiichi TAKAZAWA3, Georges Ceuleneer4, Katsuyoshi Michibayashi5, Tomoki Sato1, Shuichi Kodaira1, Seiichi Miura1 (1.Japan Agency for Maine-Earth Science and Technology, 2.Japan Coast Guard, 3.Niigata University, 4.Universite de Toulouse, 5.Nagoya University)
*FLORENCE ANNETTE CRUSPERO LABIS1, BETCHAIDA D PAYOT1, GABRIEL THEOPHILUS V VALERA1, JULIUS A PASCO1, JESLEY MEI A DYCOCO1 (1.UNIVERSITY OF THE PHILIPPINES)
*Chris Conway1, Kenichiro Tani2 (1.Geological Survey of Japan, 2.National Museum of Nature and Science)