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Ogg, James G; Robertson, Alastair H F; Jansa, Lubomir F (1983): (Table 7) Microfacies of DSDP Hole 76-534A lime-rich turbidites (Oxfordian-late Callovian) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.810026, In supplement to: Ogg, JG et al. (1983): Jurassic sedimentation history of Site 534 (western North Atlantic) and of the Atlantic-Tethys Seaway. In: Sheridan, RE; Gradstein, FM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 76, 829-884, https://doi.org/10.2973/dsdp.proc.76.141.1983

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Project(s):
Coverage:
Latitude: 28.343300 * Longitude: -75.381700
Date/Time Start: 1980-10-21T00:00:00 * Date/Time End: 1980-10-21T00:00:00
Minimum Elevation: -4971.0 m * Maximum Elevation: -4971.0 m
Event(s):
76-534A * Latitude: 28.343300 * Longitude: -75.381700 * Date/Time: 1980-10-21T00:00:00 * Elevation: -4971.0 m * Penetration: 1666.5 m * Recovery: 612.4 m * Location: North Atlantic/BASIN * Campaign: Leg76 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 127 cores; 1113.1 m cored; 31.5 m drilled; 55 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelOgg, James GDSDP/ODP/IODP sample designation
Lithology/composition/faciesLithologyOgg, James G
BioclastsBioclastsOgg, James G
Minor components/lithologyMin compOgg, James GSilt-sized components
CommentCommentOgg, James G
Size:
85 data points

Data

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Sample label

Lithology

Bioclasts

Min comp

Comment
76-534A-115-1,12Marly pelmicrite limestoneCalcified radiolarians (rare), shell fragments (rare)Quartz (6), mica (3), pyrite, opaques (tr)Micrite has a pelletoid texture
76-534A-115-1,17Marly micriteNoneQuartz (5), clastic calcite (5), mica (3), opaques (2), phosphate (rare)Calcite is 20-30 µm, with no identifiable biogenic origin; Chondrites burrows are filled by clay
76-534A-116-1,70Radiolarian biomicriteCalcified radiolarians (30)Opaques (1-2)Radiolarians are spar or microspar filled; no pyrite
76-534A-118-1,19BiomicriteCalcified radiolarians (7), echinoderm plates (3), shell fragments (2)Pyrite, phosphate (rare)Micrite has a pelletoid or clotted texture
76-534A-118-1,29Laminated pelmicriteEchinoderm plates (4), shell fragments (2), benthic foraminifers (rare)Phosphate (rare)Pelletoid texture; laminae are more porous, with interlocking grains of calcite
76-534A-118-1,83Sparse biomicriteCalcified radiolarians (6), shell fragments (rare)Quartz, mica (rare)Dense micrite; bioturbated
76-534A-120-1,44Marly micriteNoneClastic calcite (2), organics (4), quartz, phosphate, and pyrite (rare)Top of turbidite; clay and amorphous organics increase toward top
76-534A-120-1,48Bioclastic pelmicriteSilicified radiolarians (17), shell fragments (9), echinoderm plates (2)Pyrite (rare)Well-sorted mix of micrite pelets, quartz-replaced radiolarians, and shell filaments, coarse-grained base of turbidite
76-534A-121-1,6Marly micriteNoneQuartz (2), mica (3), opaques (3)Top of turbidite; Chondrites burrows are clay-rich; there is a sharp upper contact with claystone
76-534A-121-1,26Radiolarian biomicritePyrite-replaced radiolarians (11), Calcified radiolarians (6), shell fragments (3)Pyrite, phosphate (rare)Middle of a thick (45 + cm) turbidite
76-534A-122-1,2Pelmicrite and bioclastic pelletal microspariteRadiolaria, calcified (up to 7), shell filaments (1), benthic foraminifers (1), calcispheres (rare)Quartz (up to 6), pyrite, phosphate (1), pellets (30-50 µm) (35)Base of turbidite; concentration of bioclasts in microspar at base; lamination is caused by variable pellet density-size
76-534A-122-1,67Marly bioclastic pelmicriteFine shell fragments (8), pyritized radiolarians (2), echinoderm debris, calcispheres (1)Quartz (rare)Middle of turbidite; pelletoid texture
76-534A-122-2,41Marly micriteNoneOrganics (6), quartz (4), mica (2), clastic calcite (2),Top of turbidite; becomes very clay-rich towards top
76-534A-122-2,50Marly biomicriteShell filaments (6), calcified radiolarians (1), calcified ostracode (one)Pyrite (4)Vaguely pelletal texture
76-534A-123-4,25Bioclastic pelmicriteShell filaments (5), echinoderm debris (2), Pyrite-replaced, calcitefilled radiolarians (2), foraminifers, calcispheres (rare)Quartz (1), phosphate (1), pyrite (1)Base of turbidite; 30% micrite pellets; matrix is microspar in places
76-534A-124-1,10Bioclastic pelmicriteShell filaments (10) pyritized radiolarians (1)Quartz (2), phosphate (rare)Base of turbidite; 40% micrite pellets; rare clay seams
76-534A-125-1,46MicriteNoneQuartz (1), pyrite, organics (1)Top of turbidite; Chondrites burrows are micrite-filled