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Volumn 69-70, Issue , 2000, Pages 53-57

Porefluid evolution in the Kimmeridge Clay Formation of the UK Outer Moray Firth

Author keywords

Concretions; Diagenesis; Overpressure; Porosity

Indexed keywords

CONCRETIONS; DIAGENESIS; OVERPRESSURE; POREFLUID EVOLUTION; VITRINITE REFLECTANCE MODEL;

EID: 0034210421     PISSN: 03756742     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0375-6742(00)00044-3     Document Type: Conference Paper
Times cited : (7)

References (9)
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  • 2
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    • Isotopic evidence for source of diagenetic carbonates formed during burial of organic rich sediments
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    • McCants, C.Y., Burley, S.D. 1996. Reservoir architecture and diagenesis in downthrown fault block plays: the Lowlander Prospect of Block 14/20b, Witch Ground Graben, Outer Moray Firth, UK North Sea. In: A. Hurst et al. (Eds.), Geology of the Humber Group: Central Graben and Moray Firth, UKCS, Geol. Soc. Spec. Publ. No. 114, pp. 251-285.
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  • 7
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    • Scotchman I.C. Diagenetic pore fluid evolution in the Kimmeridge Clay Formation: from concretions to sandstone cements. Manning D.A.C., Hall P.L., Hughes C.R. Geochemistry of Clay-Pore Fluid Interactions. 1993;127-159 Chapman and Hall, London. Minerlogical society special publication.
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.