Estimation of emplacement depth for the Miocene Kaikomagatake granitoid pluton: constraints on crustal denudation history of the Izu collision zone
Author:
Affiliation:
1. Department of Earth Sciences, Faculty of Science, Ehime University
2. Department of Earth Sciences, Graduate School of Science and Engineering, Ehime University
3. Division of Mineral Sciences, National Museum of Nature and Science
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/115/3/115_191031/_pdf
Reference53 articles.
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2. Asano, S., Wada, K., Yoshii, T., Hayakawa, M., et al (1985) Crustal structure in the northern part of the Philippine Sea plate as derived from seismic observations of Hatoyama–Off Izu Peninsula explosions. Journal of Physics of the Earth, 33, 173–189.
3. Bando, M., Bignall, G., Sekine, K. and Tsuchiya, N. (2003) Petrography and uplift history of the Quaternary Takidani Granodiorite: could it have hosted a supercritical (HDR) geothermal reservoir? Journal of Volcanology and Geothermal Research, 120, 215–234.
4. Dodson, M.H. and McClelland–Brown, E. (1985) Isotopic and palaeomagnetic evidence for rates of cooling, uplift and erosion. Geological Society, London, Memoirs, 10, 315–325.
5. Dou, J.–Z., Zhang, H.–F., Tong, Y., Wang, F., et al (2018) Application of geothermo–barometers to Mesozoic granitoids in the Jiaodong Peninsula, eastern China: Criteria for selecting methods of pressure estimation and implications for crustal exhumation. Journal of Asian Earth Sciences, 160, 271–286.
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