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(Table 1) Magnetic properties of sediments at DSDP Holes 92-597B and 92-597C
Measurements of magnetic properties were made on basalt samples recovered from Holes 597B and 597C. This paper describes the intensity and inclination of natural remanent... -
(Table T1) Radioelement concentration and radiogenic heat production of ODP H...
Mean values of radiogenic heat production are derived from measurements of radioelements on the following rock types: amphibolite (0.358 ± 0.118 µW/m3) and tonalite gneiss... -
(Table T1) Geochemical composition of tochilinite and related minerals of ODP...
Tochilinite (approximately FeS(Mg,Fe)(OH)2) is locally abundant in Hole 1068A serpentinites from Cores 173-1068A-21R and 22R. It occurs in veins, as fillings in void space, and... -
(Table T1) Geochemical composition of gabbroic rocks from ODP Hole 176-735B
Elemental data for 89 whole-rock samples from Hole 735B, 500-1500 meters below seafloor (Ocean Drilling Program Leg 176), are presented. The samples represent the rock types... -
(Table T1) Orientation estimates for oxide-bearing lithologies of ODP Hole 17...
During a lull in hammer drill testing during Ocean Drilling Program Leg 179, Hole 1105A was cored to 158 mbsf on the Southwest Indian Ridge within ~1.3 km of Hole 735B. This... -
(Table T1) Magnetic anisotropy of samples from ODP Hole 180-1117A
At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a fault zone and recovered fault gouge, mylonitized and brecciated gabbros,... -
(Table T1) Major and trace element concentrations of whole-rock samples from ...
Skiff Bank is a bathymetric and gravimetric high located ~350 km southwest of the Kerguelen Islands in the northern portion of the Kerguelen Igneous Province (KIP). Ocean... -
(Table T1) Physical properties of minicores from ODP Leg 193 sites, PACMANUS ...
Permeability of the ocean crust is one of the most crucial parameters for constraining submarine fluid flow systems. Active hydrothermal fields are dynamic areas where fluid... -
(Table T1) Geochemistry of anhydrite separates from hydrothermal veins and vu...
Sr and S isotope data as well as trace element data for anhydrite samples from Sites 1188 and 1189 in the PACMANUS hydrothermal area are presented here. 87Sr/86Sr ratios range... -
(Tables T1, T2) Major element content in alteration categories of ODP Site 19...
In the Ocean Drilling Program's only foray to an active seafloor hydrothermal system hosted by felsic volcanic rocks at a convergent plate margin, deep penetrations were... -
(Table T1) Natural structures measured at ODP Hole 206-1256D with respect to ...
Brittle structures (open fractures and veins) from basaltic oceanic crust drilled at Ocean Drilling Program (ODP) Site 1256 (Guatemala Basin, Pacific Ocean) during Leg 206 were... -
(Table 1) Summary of horizon, lithology, and paleomagnetic of ODP Hole 126-79...
A paleomagnetic study was made on the highly vesiculated basaltic tuff breccia (the basaltic mousse) drilled by Ocean Drilling Program Leg 126 from the Izu-Bonin backarc, Sumisu... -
(Table 1) Chemical composition of hydrous and other minerals and their chromi...
This dataset has no description
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(Table 1) Chemical composition of hydrous and other minerals and their chromi...
This dataset has no description
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(Table 1) Intensities and directions of natural remanent magnetization, initi...
This dataset has no description