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- W2141503676 abstract "Progressive change in the ratio of the weight percentage of the anion radical to the cation radical as the fundamental control of sequence in deposition of minerals is the basic thesis of this paper. Evidence is given showing that oxide minerals are deposited in an ideal or sequence in such order that each mineral has a larger weight percentage in the anion radical than the next older mineral; sulphides are deposited after oxides with each younger sulphide having a smaller weight percentage in the anion radical than the next older mineral. Textures as a means of determining age relationships are discussed. Actual sequences of various classes of ore deposits are given and compared with the theoretical normal sequence." @default.
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- W2141503676 date "1940-05-01" @default.
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- W2141503676 title "A theory of mineral sequence in hypogene ore deposits" @default.
- W2141503676 doi "https://doi.org/10.2113/gsecongeo.35.3.359" @default.
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