Crystal Chemistry of Amphibole Minerals in Extraterrestrial Materials and Implications for Their Formation History

• MIKOUCHI Takashi

  Department of Earth and Planetary Science, University of Tokyo

• MONKAWA Akira

  Tokyo Metropolitan Industrial Technology Research Institute

• SUGIYAMA Kazumasa

  Institute of Materials Research, Tohoku University

Bibliographic Information

Other Title

• 鉱物結晶学の多様化：新たな広がりと挑戦　　３．宇宙鉱物（地球外物質）地球外試料中角閃石の結晶化学と形成過程について
• 地球外試料中角閃石の結晶化学と形成過程について
• チキュウ ガイ シリョウ チュウカクセンセキ ノ ケッショウ カガク ト ケイセイ カテイ ニ ツイテ

Abstract

Although amphibole is one of the most common rock-forming minerals on the earth, it rarely occurs in meteorites. This is due to anhydrous and low-pressure environment of most meteorite parent bodies. In this paper we report two different occurrences of amphibole from extraterrestrial materials. One is hornblende from an R chondrite, and the other is kaersutite from Martian meteorites. Both amphiboles bear unique crystal chemistry different from terrestrial ones and provide important information about their thermal history especially related to the water in extraterrestrial environment.

Journal

• Nihon Kessho Gakkaishi

  Nihon Kessho Gakkaishi 53 (1), 64-69, 2011

  The Crystallographic Society of Japan

Details

• CRID: 1390282679062326272
• NII Article ID: 10027840618
• NII Book ID: AN00188364
• DOI: 10.5940/jcrsj.53.64
• ISSN: 18845576
• ISSN: 03694585
• NDL BIB ID: 11029215
• Web Site: http://id.ndl.go.jp/bib/11029215
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I11029215
• Text Lang: ja
• Data Source:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
  • KAKEN
• Abstract License Flag: Disallowed