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(Tables 1-2) Petrographic features, chemical and isotopic data for leached an...
This dataset has no description
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(Table 4) Pb-, Sr- and O-isotopic compositions, and Rb and Sr contents of som...
Oxygen isotopic measurements were carried out at the University of Tuebingen, using splits of the whole-rock powders analyzed for Sr. Oxygen was extracted using the bromine... -
Description of lithologic section units of IODP Hole 357-M0076B
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0076A
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0075B
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0075A
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0072B
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0072A
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0069A
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0068B
This dataset has no description
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Description of lithologic section units of IODP Hole 357-M0068A
This dataset has no description
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(Table 1) Sulfur isotopes, total sulfur, and degree of oxidation of basalt sa...
Whole-rock basalt samples from the upper half of Deep Sea Drilling Project Hole 504B have oxygen-isotope compositions typical of mid-ocean-ridge basalts which have experienced a... -
(Table 2) Representative major and trace element analyses of diabase dikes of...
Hole 504B is located in Panama Basin approximately 200 km south of the Costa Rica Rift within a tectonically undisturbed oceanic crust formed at the Costa Rica Rift spreading... -
(Table 1) Oxygen and hydrogen isotope ratios of hydrothermal altered dolerite...
Dolerite samples, recovered in the dike complex between 1589 and 1991 meters below seafloor in Hole 504B during Legs 137/140, have been altered by hydrothermal fluids as shown... -
(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... -
(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... -
Curie temperatures and cell edges of ODP Leg 120 samples (Table 1)
Basalt samples recovered on Ocean Drilling Program Leg 120 from the Kerguelen Plateau were investigated by thermomagnetic analysis, X-ray diffraction, and ore microscopy. The... -
Petrologic description and values of resistivity, CEC, and porosity of sample...
The resistivity, porosity, and cation exchange capacity of 36 basaltic samples recovered in Hole 504B during four DSDP and ODP legs have been measured in the laboratory at room... -
(Table 1) Lithium concentration and isotopic composition of rocks from ODP Ho...
Sr and d18O data see Teagle et al. (1996) datasets: doi:10.1594/PANGAEA.713424 -
87Sr/86Sr ratios, Sr and Rb concentrations and stable oxygen isotope values f...
Seventeen whole-rock samples, generally taken at 25-50 m intervals from 5 to 560 m sub-basement in Hole 504B, drilled in 6.2 m.y. old crust, were analysed for 87Sr/86Sr ratios,...
