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Magnetic susceptibility in the Blue Lias Formation from Pinhay Bay to West Cl...
-9999 = missing values, NA = Not applicable or not available. -
Magnetic susceptibility in the Blue Lias Formation from St Audries Bay, Somerset
-9999 = missing values, NA = Not applicable or not available. -
Magnetic susceptibility in the Blue Lias Formation from Southam Quarry, Warwi...
-9999 = missing values, NA = Not applicable or not available. -
Magnetic susceptibility in the Blue Lias Formation from Quantocks Head, Somerset
-9999 = missing values, NA = Not applicable or not available. -
Magnetic susceptibility in the Blue Lias Formation from St Marys Well Bay, La...
-9999 = missing values, NA = Not applicable or not available. -
(Table S2) Peat properties for cores including sampling depths, bulk density,...
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(Table S1) Geochemical composition of tephra from sediment core DA04-31P
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(Table 1) Whole-rock major element and nickel chemistry of the relatively fre...
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(Table DR2) Chlorine concentration and isotopic data for serpentine seamount ...
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(Table DR2) Chlorine concentration and isotopic data for serpentine seamount ...
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(Table DR2) Chlorine concentration and isotopic data for serpentine seamount ...
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(Table DR2) Chlorine concentration and isotopic data for serpentine seamount ...
This dataset has no description
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(Table DR2) Chlorine concentration and isotopic data for serpentine seamount ...
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(Table DR2) Chlorine concentration and isotopic data for serpentine seamount ...
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(Appendix) Sample description of DSDP Leg 37
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(Table 2) Chlorine geochemistry and mineralogy of altered oceanic crust samples
Bulk chlorine concentrations and chlorine stable isotope compositions were determined for hydrothermally altered basalt (extrusive lavas and sheeted dikes) and gabbro samples (n... -
(Table 1) Basement penetration, recovery, and lithology of crustal DSDP holes...
Oceanic crustal drilling by R. V. Glomar Challenger at 15 sites in the North Atlantic has led to a complex picture of the upper half kilometer of the crust. Elements of the... -
(Table 1) Composition of DSDP Hole 37-334 clinopyroxenes
Recent studies of abyssal peridotites (Johnson et al., 1990, doi:10.1029/JB095iB03p02661), mid-ocean-ridge basalts (MORBs) (McKenzie, 1985, doi:10.1016/0012-821X(85)90001-9) and... -
The distribution of sulfur in oceanic crust with respect to oxidative diagene...
A detailed geochemical-petrological examination of layer 2 basalts recovered during Leg 37 of the DSDP has revealed that the original distribution, form and abundance of igneous... -
Composition of chromian diopside megacryst in DSDP Leg 37 basalts (Table 2, 3)
Refractory megacrysts of olivine, plagioclase, chromian diopside and Cr-Al spinel, which were not in equilibrium with the host oceanic tholeiite on eruption, are present in...