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Innumerous tiny pyrite granules of various shape were found in the calcareous concretions of the Upper Cretaceous formations of Sakhalin and Hokkaido. The framboidal pyrite mostly replenishing in the ...tests of diatoms, foraminifers and radiolarians occurs in the majority of these granules. A reconsideration on the origin of the framboidal pyrite is given in the present paper, although it was discussed in some details in the previous paper (KATO, 1967).続きを見る
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Mendeley出力
20_01_p073