Middle Jurassic great oolite of southern England, facies development and regional significance of dedolomitization during basin evolution

Conference · Fri May 01 04:00:00 EDT 1987 · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)

OSTI ID:5782213

Sellwood, B W; Evans, R

The oolitic and skeletal grainstones and packstones of the Great Oolite accumulated as a southward-prograding ramp sequence adjacent to both the emergent London-Brabant Massif and the rift-related swamps of the North Sea. Both at outcrop and in the subsurface, complete transitions are seen from lignitic terrestrial facies, through muddy restricted shelf to open-water grainy associations. The latter facies provide major reservoir targets in south England. Southward, below south England, grainstones give way to oncolitic packstones and eventually to basinal mudstones. Minor coral-rich thickets occur sporadically in back-shoal settings. The Great Oolite shelf prograded as two major regressive limestone units, each separated by a minor but regionally extensive transgressive unit. Temporary, and some extensive, phases of exposure led to the generation of early meteoric diagenetic features. In contrast to its outcrop character, the Great Oolite in the subsurface is often extensively dolomitized. Dolomite occurs in two forms: (1) as finely crystalline rhombs replacing original micrite and (2) as weakly ferroan saddle (or baroque) dolomite. Saddle dolomite occurs within primary pores, secondary intergranular and intragranular pores, as intergranular displacive crystals, within fractures, and locally replacing ooids and ferroan calcite cements. Microrhombic dolomite represents an early phase of mixing zone dolomitization. Saddle dolomite was emplaced at a late stage during deeper burial and at temperatures well in excess of 55/sup 0/C. Saddle dolomite precipitated from ferroan waters derived from compacting shales within deeper parts of the basins. Saddle dolomite is frequently replaced (both partially and wholly) by mildly ferroan calcite (dedolomitization).

• Research Organization: Univ. of Reading, England
• OSTI ID: 5782213
• Report Number(s): CONF-870606-
• Conference Information: Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Journal Volume: 71:5
• Country of Publication: United States
• Language: English

Related Subjects

02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
ALKALINE EARTH METAL COMPOUNDS
CALCIUM CARBONATES
CALCIUM COMPOUNDS
CARBON COMPOUNDS
CARBONATE MINERALS
CARBONATE ROCKS
CARBONATES
DIAGENESIS
DOLOMITE
EUROPE
GEOLOGIC AGES
JURASSIC PERIOD
MAGNESIUM CARBONATES
MAGNESIUM COMPOUNDS
MESOZOIC ERA
MINERALS
OXYGEN COMPOUNDS
ROCKS
SEDIMENTARY ROCKS
UNITED KINGDOM
WESTERN EUROPE