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(Table 3) Mineral proportions and serpentine polymorphs of selected DSDP and ...
Sediment depth is given in mbsf. <0.1 = traces. -
(Table 1) Description of DSDP and ODP serpentinite core samples
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(Table 1) Sample description of ODP Hole 118-735B
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(Table 4) Age determination and argon isotope ratios of igneous rocks of ODP ...
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(Table 1) List of samples collected in the field of Tersang gold deposit
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(Table 1) Rock type and summary of alteration after component minerals in thi...
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(Table 1) B content, d11B, δ¹⁸O, degree of alteration, and lithology of basal...
Boron contents and boron isotopic compositions were determined for the uppermost 1.3 km section of typical 6.2 Ma oceanic crust from DSDP/ODP Hole 504B, Costa Rica Rift,... -
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,... -
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... -
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... -
(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) 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... -
(Appendix A) Sulphur isotope ratios of upper crust samples of the sheeted dyk...
The behaviour of seawater sulphate in hydrothermal systems at intermediate- to fast-spreading ridges is investigated using new analyses of the d34S, sulphur concentration and... -
(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 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... -
Description of lithologic section units of IODP Hole 357-M0069A
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Description of lithologic section units of IODP Hole 357-M0068B
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Description of lithologic section units of IODP Hole 357-M0068A
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Description of lithologic section units of IODP Hole 357-M0075A
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Description of lithologic section units of IODP Hole 357-M0072B
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