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(Table 1) Interstitial water chemistry at DSDP Leg 76 Holes
Low salinities and strong opposing fluctuations between chlorinity and interstitial water d18O and dD characterize the region of gas-hydrate occurrence at Site 533. In addition... -
(Table 1) Geochemistry at DSDP Hole 76-534A
Mineralogical and geochemical investigations carried out on Callovian to upper Cenozoic basalt and sediments of Hole 534A are the bases for paleoenvironmental interpretations.... -
Interstitial water chemistry of Hole 76-533A
Details given in volume 76, chapter 14 -
Interstitial water chemistry of Hole 76-533
Details given in volume 76, chapter 14 -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Magnetic properties of Cenozoic MORB and Cretaceous MORB from DSDP and ODP holes
The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt (MORB) samples shows systematic variations as a function of age has long been... -
Total calcareous nannofossils abundance and accumulation rates over the past ...
This dataset has no description
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Correlation of Late Jurassic and Early Cretaceous zonation events in ODP and ...
A database was built of 378 stratigraphic events, including first and last stratigraphic occurrences (FO/LO) of calcareous nannofossils, foraminifers, and dinocysts, and... -
(Table 3) Gas hydrates collected within the Blake Ridge region, DSDP/ODP data
The Blake Ridge region lies on the passive margin of southeastern North America and contains a large amount of methane gas hydrate. The methane and methane gas hydrate are... -
Cenozoic radiolarians from the Bahamas
Radiolarians from two sites north of Little Bahama Bank (Sites 627 and 628) are correlated with assemblages from sites on the southeastern U.S. coastal plain and continental... -
Rock eval analysis of organic material from DSDP Hole 76-533A
This dataset has no description
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Thickness and duration of biostratigraphic zones, assemblages, ages and sedim...
In this Initial Report of the Deep Sea Drilling Project, detailed studies of Sites 533 (gas hydrates) on the Blake Outer Ridge and 534 (oldest ocean history) in the Blake-Bahama... -
Jurassic sedimentation history at DSDP Hole 76-534A
Site 534 reflects a complex interplay of global, basinal, and local influences on sedimentation during the Callovian and Late Jurassic. Rifting and rapid subsidence of the... -
Sedimentology and origin of lower Cretaceous pelagic carbonates and redeposit...
Drilling at Site 534 in the Blake-Bahama Basin recovered 268 m of Lower Cretaceous, Berriasian to Hauterivian, pelagic carbonates, together with volumetrically minor... -
Geochemistry at DSDP Hole 76-534A
At Site 534 in the Blake-Bahama Basin, western North Atlantic, an interval of 68 m of Maestrichtian (Upper Cretaceous) and upper middle to upper Eocene sediments consists of... -
Geochemistry and minerals at DSDP Hole 76-534A
Leg 76 sampled 31.5 m of basaltic basement at Deep Sea Drilling Project Hole 534A in the Blake-Bahama Basin. The basalts represent a short section of mineralogically uniform,... -
Susceptibility and time-dependent magnetization of basalts at DSDP Hole 76-534A
Basalts from Hole 534A are among the oldest recovered from the ocean bottom, dating from the opening of the Atlantic 155 Ma. Upon exposure to a 1-Oe field for one week, these... -
Calcareous nannofossil zonation, ages and sedimentation rates at DSDP Hole 76...
A zonation is presented for the oceanic late Middle Jurassic to Late Jurassic of the Atlantic Ocean. The oldest zone, the Stephenolithion bigotii Zone (subdivided into a... -
Carbonate, organic carbon, pyrolysis and composition of the extracts at DSDP ...
The geochemical studies of Sites 534 and 391 and their comparison allow us to improve the chemical characterization of different geological formations dating from the early... -
Lithology and organic geochemistry at DSDP Hole 76-534
The organic facies of Early and middle Cretaceous sediments drilled at DSDP Site 534 is dominated by terrestrially derived plant remains and charcoal. Marine organic matter is...
