[R7-11] The magmatic conditions and hypersolidus deformation of lower crustal magma chamber below a fast-spreading ridge. Insight from the core analyses of the Oman ICDP drill holes GT1A and GT2A | 一般社団法人日本鉱物科学会2022年年会・総会

一般社団法人日本鉱物科学会2022年年会・総会

2022年9月17日〜9月19日新潟大学五十嵐キャンパス

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一般社団法人日本鉱物科学会2022年年会・総会

2022年9月17日〜9月19日新潟大学五十嵐キャンパス

[R7-11]The magmatic conditions and hypersolidus deformation of lower crustal magma chamber below a fast-spreading ridge. Insight from the core analyses of the Oman ICDP drill holes GT1A and GT2A

*Trinh Nguyen¹, Susumu Umino¹, Takahiro Fudai³, Yuki Kusano², Osamu Ishizuka², Akihiro Tamura¹, Tomoaki Morishita¹(1. Kanazawa University, 2. AIST, 3. Pacific Cement, Co. Ltd.)

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The ICDP Oman Drilling Project drilled the lower crustal section of the Oman Ophiolite in Wadi Gideah, north of Ibra and recovered 400 m long cores each from Hole GT1A and GT2A. Microscope observations and La-ICP-MS analyses were conducted on the core samples to obtain microstructural data and trace element concentrations, which help to understand the magmatic conditions and hypersolidus deformation operated in the lower crustal magma chamber beneath the Oman paleoridge axis.

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