-
P-wave velocity (PWS split-core system) on ODP Hole 193-1188A
This dataset has no description
-
Thermal conductivity of ODP Hole 193-1191A
This dataset has no description
-
Thermal conductivity of ODP Hole 193-1190B
This dataset has no description
-
Thermal conductivity of ODP Hole 193-1189B
This dataset has no description
-
Thermal conductivity of ODP Hole 193-1189A
This dataset has no description
-
Thermal conductivity of ODP Hole 193-1188F
This dataset has no description
-
Thermal conductivity of ODP Hole 193-1188A
This dataset has no description
-
Raw data files of X-ray diffraction analysis from ODP Hole 193-1190C
X-ray diffraction data stored as flat files in a zip archive. -
Raw data files of X-ray diffraction analysis from ODP Hole 193-1188B
X-ray diffraction data stored as flat files in a zip archive. -
(Table S1) Trace element and isotopic compositions of anhydrites sampled in t...
Microchemical analyses of rare earth element (REE) concentrations and Sr and S isotope ratios of anhydrite are used to identify sub-seafloor processes governing the formation of... -
(Table T1) Permeability, electrical resistivity and density of ODP Hole 193-1...
Magmatic fluids, heat fluxes, and fluid/rock interactions associated with hydrothermal systems along spreading centers and convergent margins have a significant impact on the... -
(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... -
(Table T1) Geochemical composition of xenoliths and host rocks from ODP Hole ...
A number of intensely altered, dark xenoliths with palimpsest quench textures were recorded within altered dacitic host rocks at Site 1189 (Roman Ruins, PACMANUS) during Ocean... -
(Table T1) Geochemistry of borehole fluids from ODP Site 193-1188 and Hole 19...
Four samples of borehole fluid collected with the Water Sampling Temperature Probe at the PACMANUS hydrothermal during Leg 193 were all significantly diluted by entrained... -
(Table T1) Bulk rock geochemistry of fresh lavas from ODP Leg 193 sites, PACM...
Leg 193 was the fourth Ocean Drilling Program expedition focusing on understanding subseafloor hydrothermal systems. This program was the first to combine studies of 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... -
Rare-earth element concentration of anhydrite vein separated from ODP Site 11...
Ocean Drilling Program (ODP) leg 193 successfully drilled four deep holes (126 to 386 m) into basement underlying the active dacite-hosted Pacmanus hydrothermal field in the... -
Hole/Core summary of ODP Site 193-1191
This dataset has no description
-
Hole/Core summary of ODP Site 193-1190
This dataset has no description
