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- W1997006938 abstract "Slightly and moderately deformed palagonitic rocks from Jamaica suggest the destiny of palagonite. The principal rock described indicates its origin in sideromelane tuff, gives evidence of a palagonite-tuff stage, and displays in detail its mode of deformation. Sideromelane is inherently unstable; and palagonite, the product of the action of water upon it, is essentially chlorite. But palagonitization is slow, and, before it is much advanced, the rock spaces have usually been filled with low-grade chlorite followed by zeolite. The deposition of chlorite is often in two stages, which may differ entirely in orientation. Deformation, facilitated by the low resistance, raises the grade of both these chlorites; and chlorite schists and chlorite and albite schists, it is suggested, largely result from the dynamometamorphism of palagonite tuffs." @default.
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- W1997006938 date "1943-05-01" @default.
- W1997006938 modified "2023-09-27" @default.
- W1997006938 title "Some Altered Palagonite Tuffs from Jamaica and the Origin and History of Their Chlorites" @default.
- W1997006938 doi "https://doi.org/10.1086/625147" @default.
- W1997006938 hasPublicationYear "1943" @default.
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