Reference Type | Journal (article/letter/editorial) |
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Title | Sediment–sea-water interaction at 200 and 300 °C, 500 bars pressure: The role of sediment composition in diagenesis and low-grade metamorphism of marine clay |
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Journal | Geological Society of America Bulletin |
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Authors | THORNTON, EDWARD C. | Author |
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SEYFRIED, WILLIAM E. | Author |
Year | 1985 | Volume | 96 |
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Issue | 10 |
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Publisher | Geological Society of America |
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DOI | doi:10.1130/0016-7606(1985)96<1287:siaacb>2.0.co;2Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 53934 | Long-form Identifier | mindat:1:5:53934:8 |
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GUID | 0 |
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Full Reference | THORNTON, EDWARD C., SEYFRIED, WILLIAM E. (1985) Sediment–sea-water interaction at 200 and 300 °C, 500 bars pressure: The role of sediment composition in diagenesis and low-grade metamorphism of marine clay. Geological Society of America Bulletin, 96 (10) 1287 doi:10.1130/0016-7606(1985)96<1287:siaacb>2.0.co;2 |
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Plain Text | THORNTON, EDWARD C., SEYFRIED, WILLIAM E. (1985) Sediment–sea-water interaction at 200 and 300 °C, 500 bars pressure: The role of sediment composition in diagenesis and low-grade metamorphism of marine clay. Geological Society of America Bulletin, 96 (10) 1287 doi:10.1130/0016-7606(1985)962.0.co;2 |
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In | (1985) Geological Society of America Bulletin Vol. 96 (10) Geological Society of America |
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