Mineralogical alteration of CM carbonaceous chondrites: A view

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概要

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• CM carbonaceous chondrites have been considerably affected by aqueous alteration, probably on the regolith of their parent body or bodies. The aqueous alteration resulted in the alteration of anhydrous silicates, metal, and sulfides, producing a complex mixture of Fe-Mg serpentines, Fe-Ni-S-O phase (tochilinite), and minor Fe-rich oxides and Fe-Ni sulfides. We here present a review of recent petrographic and mineralogical studies of CM carbonaceous chondrites and interpretations of their mineralogical alteration process.

• 国立極地研究所の論文

著者

• Tomeoka Kazushige

  Mineralogical Institute Faculty Of Science University Of Tokyo

• Buseck Peter

  Department Of Geology And Chemistry Arizona State University

• McSween Harry

  Department of Geological Sciences, University of Tennessee

• Mcsween Harry

  Department Of Earth & Planetary Sciences University Of Tennessee

• Mcsween Harry

  Department Of Geological Sciences University Of Tennessee

関連論文

• Yamato-86720: A CM carbonaceous chondrite having experienced extensive aqueous alteration and thermal metamorphism
• Yamato-82162: A new kind of CI carbonaceous chondrite found in Antarctica
• Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica
• Mineralogical alteration of CM carbonaceous chondrites: A view
• A textural examination of the Yamato 980459 and Los Angeles shergottites using crystal size distribution analysis

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