Compaction of microfossil and clay-rich sediments

Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy

Volumn 26, Issue 1-2, 2001, Pages 59-62

  Fabricius, I L ^a  

^a TECHNICAL UNIVERSITY OF DENMARK   (Denmark)

Author keywords

[No Author keywords available]

Indexed keywords

CHALK; CLAY; COMPACTION; MICROFOSSIL;

EID: 0035090704     PISSN: 14641895     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1464-1895(01)00023-0     Document Type: Article

References (20)

1. Modelling of porosity evolution and mechanical compaction of calcareous sediments
2. Porosity variation in Cenozoic and Upper Cretaceous chalk from the Ontong Java Plateau -A discussion of image analysis data
3. Chemical and mechanical processes during burial diagenesis of chalk. An interpretation based on specific surface of deep-sea sediments
4. Chalk texture in the North Sea and the Ontong Java Plateau
5. Deformation, diagenesis and mechanical behaviour of chalk
6. Classification of carbonate rocks according to depositional texture
7. Interpretation of burial history and rebound from loading experiments and the occurence of microstylolites in the mixed sediments of Caribbean sites 999 and 1001
8. Physical property changes as a monitor of pelagic carbonate diagenesis: An empirically derived diagenetic model for Atlantic Ocean basins
9. Loading experiments on carbonate ooze and chalk from Leg 130, Ontong Java Plateau
10. Deep sea carbonates: Acoustic, physical, and stratigraphic properties
11. Rock compressibility, compaction, and subsidence in high-porosity chalk reservoir: A case study of Valhall field
12. Chalk diagenesis and its relation to petroleum exploration: Oil from chalks, a modern miracle
13. Maastrichtian and Danian strata in the south-eastern part of the Danish Basin
14. Laboratory and well-log velocity and density measurements from the Ontong Java Plateau: New in situ corrections to laboratory data for pelagic carbonates
15. Influence of heat flow on ooze/chalk cementation: Quantification from consolidation parameters in DSDP sites 504 and 505 sediments