Chondrite Shock Metamorphism History Assessed by Non-Destructive Analyses on Ca-Phosphates and Feldspars in the Cangas de Onís Regolith Breccia
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DOI: 10.3390/min9070417
Abstract: The Cangas de Onís regolith breccia is an H5-H6 ordinary chondrite that fell to Earth in 1866. It is constituted by 60% H6-H5 clasts within an H5 clastic matrix. All clasts are affected by intense… read more here.
Keywords: metamorphism; cangas regolith; breccia; shock metamorphism ... See more keywords