Morphology and evolution of Mesozoic carbonate paleoshelf edge, eastern Baltimore Canyon Trough

Conference · Thu May 01 04:00:00 EDT 1986 · Am. Assoc. Pet. Geol., Bull.; (United States)

OSTI ID:5268650

Edson, G M

Deep-water petroleum exploration on the US Atlantic continental slope provided information about a Late Jurassic-Early Cretaceous shelf-edge carbonate trend. Well data and seismic interpretation indicate a ridgelike limestone buildup of probably Valanginian age at the crest. One well, penetrating over 1200 ft of this unit, shows that the buildup consists of bioclastic grainstone, packstone, wackestone, rudstone, and possible minor boundstone. Lobate metazoans several centimeters in size may be framework elements. However, more than 80% of this unit is bioclastic debris consisting mostly of coated grains, suggesting that the buildup is dominantly a shelf-edge carbonate debris accumulation. Immediately shoreward, a topographically lower tabular facies, locally 8-10 mi wide, interfingers landward with terrigenous clastics. This back-bank carbonate facies is lithologically, biologically, and genetically similar to the shelf-edge buildup, but appears to be Berriasian-Berjocian. Overlying the back-bank unit, lithologically immature Barremian-Valanginian continental clastic rocks form a seaward-thinning wedge, whose apex meets the top of the shelf-edge carbonate bank. In places, this terrigenous unit may have covered and spilled over the buildup onto the paleoslope during the Barremian and Hauterivian. Unconformably overlying the clastic wedge, an Aptian blanketlike grainstone, packstone, and wackestone unit 200-400 ft thick contains a distinctive biotic assemblage, including calpionellids, tubiphytes, and sparse heexactinellids. It is concluded that during the aptian marine regression, the terrigenous clastic unit was beveled by erosion to its present wedge configuration. The blanketlike carbonate unit was deposited on the resulting topographic surface during the subsequent Aptian transgression.

• Research Organization: Minerals Management Service, Vienna, VA
• OSTI ID: 5268650
• Report Number(s): CONF-860624-
• Conference Information: Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:5
• Country of Publication: United States
• Language: English

Related Subjects

02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
ATLANTIC OCEAN
BALTIMORE CANYON
CARBONATE ROCKS
CONTINENTAL MARGIN
CONTINENTAL SLOPE
CRETACEOUS PERIOD
DEPOSITION
EXPLORATION
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC HISTORY
JURASSIC PERIOD
MESOZOIC ERA
MINERAL RESOURCES
PETROLEUM DEPOSITS
RESOURCES
ROCKS
SEAS
SEDIMENTARY ROCKS
SURFACE WATERS