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- W2321847224 abstract "Mineral analcite (analcime) was found in the upper Flowerpot Shale (Lower Gaudalupian, Permian), Blaine County, Oklahoma. Analcite was identified by the presence of three major peaks at 5.60 A, 3.43 A, and 2.93 A, and some minor peaks on the randomly-oriented x-ray diffractograms (Figure 1). The DTA diagram of analcite shows a broad endotherimc peak at around 280 degrees centigrade (Figure 1). As reported by Koizumi (1953), analcite (analcime) dehydrates so slowly and gradually between 200 degrees and 400 degrees centigrade that in the DTA diagrams only a broad endothermic curve is obtained without a sharp endothermic peak. The purpose of this study is to infer the possible origin of the analcite on the basis of field and laboratory data." @default.
- W2321847224 created "2016-06-24" @default.
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- W2321847224 date "1970-01-01" @default.
- W2321847224 modified "2023-09-26" @default.
- W2321847224 title "Origin of Mineral Analcite in the Upper Flowerpot Shale, Northwestern Oklahoma" @default.
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- W2321847224 doi "https://doi.org/10.2307/3627305" @default.
- W2321847224 hasPublicationYear "1970" @default.
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