Mineralogical Institute, Faculty of Science, University of Tokyo/Department of Earth Sciences, Kobe University/Ocean Research Institute, University of Tokyo/National Institute of Polar Research/Department of Geology, Faculty of Liberal Arts, Nagasaki University
抄録(英)
One Fe-rich diogenite and two polymict breccias with eucritic composition have been identified in the Yamato-75 achondrites by the electron microprobe and single crystal X-ray diffraction techniques. The Yamato-75032 diogenite, a monomict breccia, contains a low-Ca inverted pigeonite with a chemical composition close to that of Binda, and a possible primary orthopyroxene. Yamato-75011 and -75015 are polymict breccias which contain mineral and lithic clasts common to eucrites. Binda-like pyroxene fragments were found in Yamato-75015,suggesting that it may represent a variety of materials expected from our layered crust model containing diogenite, Binda-type, Moore County-type, Juvinas-type and Pasamonte-type pyroxenes from bottom to top. Yamato-74659 may be classified as a weathered pyroxene-rich ureilite, which contains the most Mg-rich uninverted pigeonite. The exsolution and shock induced twinning were not observed. Yamato-74123 is another ureilite similar to Kenna.
雑誌書誌ID
AA00733561
雑誌名
Memoirs of National Institute of Polar Research. Special issue
Mineralogical Examination of the Yamato-75 Achondrites and Their Layered Crust Model
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KJ00000011507
(3.05MB)
概要
