Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University/Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University/Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University/Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science, Tohoku University
抄録(英)
Ferropseudobrookite-silica mineral-albite-chondrule was found in an unequilibraed (L3) chondrite (ALH-77015). This is the first finding of ferropseudobrookite in chondrite. The ferropseudobrookite exhibits a weakly zonal structure. The stability field of ferropseudobrookite suggests that the chondrule should have been quenched at a temperature near 1140±10℃.
雑誌書誌ID
AA00733561
雑誌名
Memoirs of National Institute of Polar Research. Special issue