日本地球惑星科学連合2014年大会

講演情報

インターナショナルセッション(口頭発表)

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG08_29AM1] Collision, Subduction, and Metamorphic processes-II

2014年4月29日(火) 09:00 〜 10:45 311 (3F)

コンビーナ:*Ur Rehman Hafiz(Department of Earth and Environmental Sciences, Graduate School of Science and Engineering, Kagoshima University)、Tatsuki Tsujimori(Institute for Study of the Earth's Interior, Okayama University)、Kazuaki Okamoto(Faculty of Education, Saitama University)、座長:Ur Rehman Hafiz(Department of Earth and Environmental Sciences, Graduate School of Science and Engineering, Kagoshima University)、Wei Chunjing(School of Earth and Space Sciences, Peking University)

09:00 〜 09:15

[SCG08-P01_PG] Melt-Peridotite Reactions In The Upper Mantle: Geochemistry Of Peridotite And Pyroxenite From The Beni-Bousera Massif

ポスター講演3分口頭発表枠

*CHETOUANI Kamar1AMRI Isma1TARGUISTI Kamal1 (1.departement de geologie, Faculte des sciences de Tetouan. Maroc)

キーワード:Geochemistry, Beni Bousera, Pyroxenite, Peridotites

The Beni-Bousera massif contains ubiquitous pyroxenites of various types, organized into conspicuous layers ranging from 0.5 to 100 cm in thickness, hosted by peridotites. Integrated field features, petrographic observations, and geochemical analyses from 92 samples (whole rock major and trace elements data: 55 samples, microprobe data for minerals: 48 samples, and mineral trace elements data: 30 samples) from pyroxenites provide information to classify the rock types into four different groups typified as: (1) garnet pyroxenites, (2) spinel-garnet websterites, (3) spinel websterites, and (4) spinel chromium websterites. Type 1 rocks, occurring at the base of the massif, are considered as the most primitive type, garnet pyroxenites layers represent the vestiges of an old veined subcontinental lithosphere. They generally indicate temperatures <970○C (based on two-pyroxene thermometry) and a low to very low Mg# (<76%). Trace element contents show enrichment in heavy and middle rare earth elements but strong depletion in light rare earth elements (LREE). Paradoxically, the host peridotites show enrichment in LREE, which give new insights into their genesis history. Based on our field observations and geochemical results, we suggest that garnet-pyroxenite layers metasomatised the host peridotite successively by the partial melting as a consequence of subsequent heating phase(s) of the lithosphere. The magmatic event that led to the diversity and zoning of mafic layers was caused by melting of the base of thinned subcontinental lithosphere by upwelling asthenosphere, followed by infiltration of asthenospheric melts. The different groups of mafic layers record several stages of this event.