A Classification of Several Yamato-74 Chondrites
スポンサーリンク
概要
- 論文の詳細を見る
Six Yamato-74 chondritic meteorites have been classified, based on iron contents of olivines and orthopyroxenes in their small fragments. The results are as follows : Yamato-74193,-74498 and -74507 are H4-chondrites, Yamato-74367 and -74603 are L4-chondrites, and Yamato-74454 is L5-chondrite.
- 国立極地研究所の論文
著者
-
Nishida Norimasa
Chemical Analysis Center The University Of Tukuba
-
Onuma Naoki
Institute Of Chemistry The University Of Tukuba
-
Ohtsuka Yoshiro
Institute of Geoscience, The University of Tsukuba
-
Ohtsuka Yoshiro
Institute Of Geoscience The University Of Tukuba
関連論文
- Crystal chemistry of ZnS minerals formed as high-temperature volcanic sublimates : matraite identical with sphalerite
- A Classification of Several Yamato-74 Chondrites
- Origin and Evolution of Condrules Based on Na/Al-Dispersion and -Convergence in Yamato-74 Ordinary Chondrites
- A Classification of Several Yamato-74 Chondrites
- Polymorphic relation between cavansite and pentagonite : Genetic implications of oxonium ion in cavansite
- Geochemical aspects of aventurine labradorites "sunstone" with inclusions of native copper : Implication for continental-margin magmatism
- First finding of thallium-bearing ammonioleucite : A signal for the ultimate stage of the hydrothermal process and for a far-reaching effect from seawater alteration of MORB
- A new A1/Si-zoning of hydrocarbon-bearing garnet in rhyolite from Mt.Nijo, Southwest Japan
- Sr/Ca-Ba/Ca systematics in Antarctic Ca-rich achondrites and their origins
- Rapid Simultaneous 17 Elements Analysis of Some Yamato Meteorites by ICP-OES