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- W2069193886 abstract "Previous workers proposed various trace elements as geochemical indicators of reef and nonreef carbonates. Analysis of the data of Chester and Billings and Ragland shows that the concentration of some of these elements (total rock Ni, Co, Cr, V, and Ba, and acid-soluble Ni, Co, V, Pb, Ga, Cu, Fe, Mn, Zn, or K) is a function of the clay-mineral content of the rocks. This gives an energy index for the environment of deposition of the rocks and is not a direct reflection of their facies type." @default.
- W2069193886 created "2016-06-24" @default.
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- W2069193886 date "1971-01-01" @default.
- W2069193886 modified "2023-09-26" @default.
- W2069193886 title "Are There Geochemical Criteria for Differentiating Reef and Nonreef Carbonates?: GEOLOGICAL NOTES" @default.
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- W2069193886 doi "https://doi.org/10.1306/5d25cf71-16c1-11d7-8645000102c1865d" @default.
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