| 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.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
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,