Geochemistry of chromian spinels from serpentinites distributed in eastern margin of the Kanto Mountains
Author:
Affiliation:
1. AIST, Geological Survey of Japan, ResearchInstitute of Geology and Geoinformation
2. Faculty of Education, Bunkyo University
Publisher
National Institute of Advanced Industrial Science
Subject
General Medicine
Link
https://www.jstage.jst.go.jp/article/bullgsj/72/5/72_447/_pdf
Reference40 articles.
1. Arai, S. (1992) Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry. Mineralogical Magazine, 56, 173–184. 10.1180/minmag.1992.056.383.04
2. 荒井章司（1992）砕屑性クロムスピネル及び砕屑性蛇紋岩の重要性．地質学論集，no. 38，329–344．
3. 荒井章司・久田健一郎（1991）関東山地，山中白亜系石堂層中の砕屑性クロムスピネル．岩鉱，86，540–553． 10.2465/ganko.86.540
4. Arai, S., Okamura, H., Kadoshima, K., Tanaka, C., Suzuki, K. and Ishimaru, S. (2011) Chemical characteristics of chromian spinel in plutonic rocks: implications for deep magma processes and discrimination of tectonic setting. Island Arc, 20, 125–137. 10.1111/j.1440-1738.2010.00747.x
5. 原 英俊（2020）関東山地東縁部，白亜系高岡層の石灰質砂岩から得られた砕屑性ジルコンU–Pb年代．地質調査研究報告，71，509–516． 10.9795/bullgsj.71.509
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1. Oceanic rocks between the Mikabu Greenstones and the Kashiwagi Unit of the Northern Chichibu Belt in the eastern margin of the Kanto Mountains, and discussion of klippe theory;The Journal of the Geological Society of Japan;2022-09-22
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