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- W2313541041 abstract "In the Hanaoka mining area of the “Green Tuff” region, the Miocene submarine lavas and pyroclastic rocks with basaltic to andesitic compositions were recrystallized at low temperatures to form various secondary minerals. The upper metabasites are characterized by the mineral assemblage of prehnite-pumpellyite facies; i.e. chlorite+epidote+prehnite+pumpellyite, although zeolites occur in amygudules and veinlets. The microprobe data of secondary minerals, in addition to the microscopic observations, revealed the existence of several local domains with different effective bulk compositions within a single thin section. The metabasites of the upper cores (about 300m below the surface) of two drill holes also show secondary mineral assemblages of prehnite-pumpellyite facies, but those of the lower cores (at 900m depth) show actinolitebearing assemblages such as chlorite+epidote+prehnite+actinolite± pumpellyite. This indicates the transition to the prehnite-actinolite facies with increasing depth." @default.
- W2313541041 created "2016-06-24" @default.
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- W2313541041 date "1990-01-01" @default.
- W2313541041 modified "2023-09-25" @default.
- W2313541041 title "Miocene metabasites of the hanaoka area, northern akita prefecture." @default.
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- W2313541041 doi "https://doi.org/10.2465/ganko.85.257" @default.
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