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TOC, carbonate and bitumen concentrations of DSDP Holes 64-477 and 64-478 (Ta...
The bitumens of a selection of subsurface sediments from Guaymas Basin, Gulf of California, have been analyzed in order to assess the hydrothermal effects on the organic matter... -
Resistivity, porosity, grain density and CEC for samples of ODP Hole 118-735B
The resistivity, porosity, and cation exchange capacity of 29 gabbroic samples recovered in Hole 735B during Leg 118 of the Ocean Drilling Program (ODP) were measured in the... -
Age determination and sedimentation rates of ODP Hole 119-740A (Table 1)
Unconsolidated sediments recovered at Site 740 include approximately 23 m of interbedded siliceous ooze and silty clay (pebbly mud), which was tentatively assigned a late... -
(Table 1) Sapropel analysis from ODP Sites 160-964, 160-966, 160-967 and 160-969
Seventeen eastern Mediterranean Pliocene sapropels from ODP Sites 964, 966, 967 and 969, some of which are coeval, have been analysed for their geochemistry. The sapropels are... -
(Table 1) Uranium and Thorium concentrations, activity ratios and calcium car...
The geochemical behaviour of uranium and thorium in metalliferous sediments and hydrothermal deposits has been widely studied and the main results have been summarised by... -
(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... -
(Table 1) Geochemistry of ODP Hole 130-807C carbonates across the K/T boundary
Paleontological, stable isotopic, trace elemental abundance, and magnetostratigraphic studies have been performed on limestones spanning the Cretaceous/Tertiary boundary... -
(Appendix) Petrographic information, trace element and Sr isotope ratios of P...
Fluid flow through the axial hydrothermal system at fast spreading ridges is investigated using the Sr-isotopic composition of upper crustal samples recovered from a tectonic... -
(Table 3) Main results of the stress tensor inversion of selected populations...
Drilling at Site 808 (ODP Leg 131) provided an extensive record of the discrete brittle structures (small faults and shear bands) at the toe of the Nankai accretionary complex.... -
(Table T1) Major element oxide and trace element concentration of ODP Hole 17...
Sixty-three major and trace element analyses from Hole 735B reflect known characteristics of the igneous and metamorphic evolution of the oceanic crust at this site. Regular... -
(Table 1) Anisotropy of magnetic susceptibility parameters of ODP Hole 134-833B
Ocean Drilling Program (ODP) Sites 832 and 833 were drilled in the intra-arc North Aoba Basin of the New Hebrides Island Arc (Vanuatu). High volcanic influxes in the intra-arc... -
Magnetostratigraphy of DSDP Leg 94 sediments
The primary objective of DSDP Leg 94 was to obtain continuous paleoclimatic records along a roughly north-south transect in the North Atlantic. The magnetostratigraphy of 21... -
(Table 1) Microfossil events at DSDP Leg 81 Holes
Leg 81 of the DSDP drilled four sites in a small area on the southwest flank of the Rockall Plateau. The biostratigraphy of the cores is based on six groups of microfossils:... -
(Table 1) Occurrences of volcanic ash at DSDP Leg 78A Holes
Air-fall volcanic ash recovered at Deep Sea Drilling Project Sites 541, 542, and 543 on and east of the toe of the Barbados Ridge delineate middle and late Miocene, early... -
(Table 2) Carbonate chemistry and isotopes from northern Cascadia margin samples
Most authigenic carbonates previously recovered from the Cascadia slope have 87Sr/86Sr signatures that reflect shallow precipitation in equilibrium with coeval seawater. There... -
(Table 1) Thermal conductivity and water content at DSDP Hole 71-511
At Hole 511, on the margin of Maurice Ewing Bank, eastern Falkland Plateau, successful bottom hole temperature measurements were made at 52.5 and 113 meters below the seafloor.... -
(Table 1) Magnetozone boundaries at DSDP Site 68-502
Obtaining long, continuous, and undisturbed sections of unconsolidated Neogene deep sea sedimentary sections has been limited by (1) practical length of piston cores to about 30... -
(Table 1) Magnetozone boundaries at DSDP Site 68-503
The paleomagnetic measurement procedure at Site 503 was similar to that described for Site 502 (See preceding chapter). Each core section was measured with the longcore spinner... -
(Table 1) Carbon, hydrocarbons and observations at DSDP Holes 67-497 and 67-498A
Gas hydrates are icelike materials that form when specific conditions of temperature, pressure, and gas composition are simultaneously satisfied. Among the first descriptions of... -
(Table 1) Basement lithologic units at DSDP Leg 65 Holes
The principal objective of DSDP Leg 65 was to sample oceanic crust near the crest of the East Pacific Rise. The sites that we drilled, close to the mouth of the Gulf of...
