Petrology of a new basaltic shergottite: Dhofar 378
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概要
- 論文の詳細を見る
Dhofar 378 is a new basaltic shergottite, consisting mainly of pyroxenes, plagioclase glass, phosphates, titanomagnetite, and mesostasis. It is one of the most ferroan shergottites and resembles the Los Angeles shergottite. Pyroxenes show remarkable chemical zoning from 0.4 of Mg/(Mg+Fe) to less than 0.1, and their REE patterns are depleted in light REE whereas the REE pattern of the bulk Dhofar 378 is flat. All plagioclase grains in the original lithology completely melted by an intense impact shock, and the plagioclase melts crystallized fibrous plagioclase to form the rims surrounding the plagioclase melts. Then, the melts quenched as plagioclase glass to form the cores. The shock stage of Dhofar 378 is higher than that of the Los Angeles shergottite. The degree of impact shock for Dhofar 378 may be about 55-75GPa and is the highest among all known martian meteorites.
- 国立極地研究所の論文
著者
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Kimura Makoto
Department of Mathematics, Faculty of Science and Engineering, Shimane University
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Ikeda Yukio
Department Of Endocrinology Metabolism And Nephrology Kochi Medical School Kochi University
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Ikeda Yukio
Department Of Earth Sciences Ibaraki University
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TAKEDA Hiroshi
Research Institute, Chiba Institute of Technology
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Ikeda Yukio
Department Of Material And Biological Science Ibaraki University
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Suzuki Akio
Faculty of Technology, Kanazawa University
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Takeda Hiroshi
Department Of Earth And Planetary Science The University Of Tokyo
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Shimoda Gen
National Institute of Advanced Industrial Science and Technology
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Kita Noriko
National Institute of Advanced Industrial Science and Technology
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Morishita Yuichi
National Institute of Advanced Industrial Science and Technology
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Jagoutz Emil
Max-Planck-Institute fur Chemie
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Dreibus Gerlind
Max-Planck-Institute fur Chemie
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Takeda Hiroshi
Research Institute Chiba Institute Of Technology
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Ikeda Yukio
Department Of Earth Sciences Faculty Of Science Ibaraki University
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Suzuki Akio
Faculty Of Science Tohoku University
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Kimura Makoto
Department Of Applied Chemistry Graduate School Of Engineering Nagoya University
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Kimura Makoto
Department Of Material And Biological Science Ibaraki University
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Kimura Makoto
Department Of Applied Biochemistory Utsunomiya University
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Ikeda Yukio
Department Of Earth Science Faculty Of Science Ibaraki University
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Shimoda Gen
National Inst. Advanced Industrial Sci. And Technol. Tsukuba
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Suzuki Akio
Faculity of Engineering, University of Miyazaki, Miyazaki 889-2192, Japan
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