Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4718650 | Marine Geology | 2011 | 10 Pages |
Abstract
⺠The impact of diagenesis on carbonate mound sediments varies among core intervals. ⺠An interval with minima in magnetic susceptibility is topped by iron rich sediments. This is overlain by a lithified interval, low in aragonite. ⺠This succession formed during times of a fixed redox boundary in the sediment. ⺠The associated lithification pre-dates erosional processes.
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Authors
Cees van der Land, Furu Mienis, Henk de Haas, Henko C. de Stigter, Rudy Swennen, John J.G. Reijmer, Tjeerd C.E. van Weering,