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Title: Distribution, chemistry, isotopic composition and origin of diagenetic carbonates: Magnus Sandstone, North Sea

Journal Article · · Journal of Sedimentary Petrology; (United States)
OSTI ID:6513098
;  [1];  [2]
  1. Univ. of Glasgow (United Kingdom)
  2. Scottish Univ. Research and Reactor Centre, Glasgow (United Kingdom)

Diagenetic ferroan carbonates grew in the Upper Jurassic reservoir sandstones of the Magnus oilfield in porewaters which differed in composition across the field. These porewaters remained compositionally different and stratified for at least 35 M.y. Variations in carbonate chemistry across the field are attributable to these porewater variations, which resulted from displacement of marine depositional water from the crest of the field by meteoric water during late Cimmerian subaerial exposure. Original depositional facies and detrital mineralogy strongly influenced diagenetic carbonate distribution. The objective of this paper is twofold: (1) to describe the occurrence of burial diagenetic magnesian siderite and ankerite from the Magnus Sandstone, and (2) to show that variations in the elemental and isotopic geochemistry of siderite and ankerite relate to long-lived variations in the composition of the porewaters in the sandstone during diagenesis.

OSTI ID:
6513098
Journal Information:
Journal of Sedimentary Petrology; (United States), Vol. 63:1; ISSN 0022-4472
Country of Publication:
United States
Language:
English