Formation and evolution of the uppermost mantle of oceanic plate and island arc based on natural samples of ultramafic-mafic rocks
Author:
Affiliation:
1. School of Geosciences and Civil Engineering, College of Science and Engineering, Kanazawa University
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/52/1/52_230203/_pdf
Reference97 articles.
1. Andal, E.S., Arai, S. and Yumur, Jr. G.P. (2005): Complete mantle section of a slow-spreading ridge-derived ophiolite: an example from the Isabela ophiolite in the Philippines. Island Arc, 14, 272-294.
2. 荒井章司,平井寿敏,阿部なつ江 (2005):かんらん岩捕獲岩の地質学的側面:日本列島の例.岩石鉱物科学,34, 133-142.
3. 荒井章司,石丸聡子(2018):島弧上部マントルの岩石学的性質:何が固有か?地質雑,124, 551-573.
4. Arai, S., Kadoshima, K. and Morishita, T. (2006): Widespread arc-related melting in the mantle section of the northern Oman ophiolite as inferred from detrital chromian spinels. J. Geol. Soc., London, 163, 869-879.
5. Dhar, A., Ghosh, B., Bandyopadhyay, D., Morishita, T., Tamura, A., France, L., Nguyen, D.K., Boulanger, M, Kokey, M., Roy, S, and Chattopadhaya, S. (2022): The lower oceanic crust at ultraslow-spreading Southwest Indian Ridge: the inside story. Gondwana Res., 111, 223-248.
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