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- W2318017191 abstract "Both the zinc and the 650' bonanzas are deposited with closely connection in the Arikoshi syncline of the chert zone, belonging to the upper Palaeozoic formations. The mineralizing solutions formed the latter ascended along the 300' vein and the folding axis that intersected to the vein, replacing chert, but the former mainly along the intersected line of the 1060' and the 300' veins. One bonanza comes into contact with the other at upper 6th level, and they have formed a large and rich bonanza. In the zinc bonanza is pyrrhotite and marmatite dominantly deposited, the 650' bonanza consists of two bodies rich in pyrrhotite and chalcopyrite. The general successions of main minerals in those are as follows; pyrrhotite→ marmatite→pyrrliotite→chalcopyrite→galena→pyrite. Perhaps, pyrrhotite and marmatite assemblage in the boundary zone of the bonanzas suggests that the zinc bonanza deposited earlier than the 650' one." @default.
- W2318017191 created "2016-06-24" @default.
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- W2318017191 date "1954-01-01" @default.
- W2318017191 modified "2023-10-04" @default.
- W2318017191 title "On the relation of the geological structure to the mineralization in the “zinc bonanza„, Ashio mine" @default.
- W2318017191 doi "https://doi.org/10.2465/ganko1941.38.8" @default.
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