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- W2097605766 abstract "ABSTRACT Fragmentary oolites and pisolites do not necessarily indicate high energy conditions of deposition. They can readily form through weak impacts of desiccation-cracked grains under relatively low energy conditions. The similarity between the fragmentary grains and portions of oolites and pisolites bounded by desiccation cracks seems to suggest that the former are products of desiccation-cracking of oolites and pisolites." @default.
- W2097605766 created "2016-06-24" @default.
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- W2097605766 date "1975-01-01" @default.
- W2097605766 modified "2023-09-24" @default.
- W2097605766 title "Derivation of Fragmentary Oolites and Pisolites from Desiccation Cracks" @default.
- W2097605766 doi "https://doi.org/10.1306/212f6e47-2b24-11d7-8648000102c1865d" @default.
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