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Occurrence of tethyan radiolarian species in early Cretaceous sediments of OD...
During ODP Leg 123, abundant and well-preserved Neocomian radiolarians were recovered at Site 765 (Argo Abyssal Plain) and Site 766 (lower Exmouth Plateau). Assemblages are... -
Particel size distribution and microstructures of sediments from ODP Leg 205 ...
Ocean Drilling Program Legs 170 and 205 offshore Costa Rica provide structural observations which support a new model for the geometry and deformation response to the seismic... -
(Table 1) Age and depth of reflectors of the 3.5-kHz and airgun seismic recor...
DSDP cores from areas of low (Site 505) and high heat flow (Site 504 B) near the Costa Rica Rift, together with seismic profiles from the Panama Basin, have been studied to... -
(Table 1) Summary of maximum clast size and bed thickness of ODP Leg 126 samples
Subaerial debris flows, with water contents ranging from as little as 10 wt% up to no more than about 25 wt% (Pierson, 1986; Pierson and Costa, 1987), are non-Newtonian fluids... -
Core-section summary from IODP Hole 317-U1353B
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Planktonic foraminifera and microfossil composition of IODP Hole 302-M0004C
Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most... -
(Table 1) Ages of planktonic foraminiferal datums at Leg 94 Sites
The six Leg 94 sites have produced a unique data set from a north-south transect of sites, all with good paleomagnetic records, and all but one with above-average accumulation... -
(Table 2) Terrigenous, authigenic and biogenic composition of sediments at DS...
Pelagic sedimentation during the Early Cretaceous at Site 603 produced alternations of laminated marly limestone and bioturbated limestone--a facies typical of the "Blake-Bahama... -
(Table 1) Description of structures in cores at DSDP Holes 59-451, 59-448A an...
Fifteen lengths of Leg 59 cores (primarily from Hole 451 as well as from Holes 447A and 448A) exhibiting macroscopic faults were selected by Dr. R. B. Scott (Co-Chief Scientist,... -
Trace element chemistry of pyrobitumen from the Tau-Tona mine in South Africa
High-grade gold and uranium mineralization in the Witwatersrand basin is intimately associated with pyrobitumen, implying that hydrocarbons may have played a role in the genesis... -
Lithological description of sediment core GIK12336-1, NW African continental ...
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Lithological description of sediment core GIK12392-1, NW African continental ...
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Lithological description of sediment cores GIK12310-3/4, NW African continent...
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Lithological description of sediment core GIK12345-4, NW African continental ...
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Lithological description of sediment core GIK12309-2, NW African continental ...
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Lithological description of sediment core GIK12343-2, NW African continental ...
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Lithological description of sediment cores GIK12327-4/5, NW African continent...
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Lithological description of sediment core GIK12308-3, NW African continental ...
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Lithological description of sediment cores GIK12328-4/5, NW African continent...
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Lithological description of sediment cores GIK12329-4/5, NW African continent...
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