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Ekdale & Bromley, 1988
Diagenetic microlamination in chalk
Ekdale, A. A., Bromley, R. G.
DOI | 10.1306/212F8E8B-2B24-11D7-8648000102C1865D |
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Year | 1988 |
Journal | Journal of Sedimentary Research |
Volume | 58 |
Number | 5 |
Type | article in journal |
Language | English |
Id | 50381 |
Abstract
The Maastrichtian chalk of Denmark contains units that exhibit a very fine lamination of presumed diagenetic origin. The chalk laminae, only a few tens or hundreds of microns thick, are bounded by irregularly wrinkled, parallel, pressure-solution planes. These appear to be microstylolitic seams that contain no detectable films of clay or other insoluble material. They possibly represent a stratigraphic condensation of up to 15%. Despite the release of considerable amounts of calcium carbonate in solution, the chalk has remained poorly cemented.
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