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Pore water saturation index at Hole 310-M0022A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0025A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Heavy mineral composition of 0.100-0.050 mm size fraction from bottom sedimen...
Data in the Ti min column show contents of indefinite titanium minerals. -
Heavy mineral composition of 0.100-0.050 mm grain size fraction from Kara Sea...
This dataset has no description
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Heavy mineral composition of 0.100-0.050 mm grain size fraction of sediments ...
This dataset has no description
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Heavy mineral composition of 0.100-0.050 mm grain size fraction of sediments ...
This dataset has no description
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Heavy mineral composition of 0.100-0.050 mm grain size fraction of sediments ...
This dataset has no description
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Heavy mineral composition of 0.100-0.050 mm size fraction of sediments from H...
This dataset has no description
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Heavy mineral composition of 0.100-0.050 mm size fraction of sediments from H...
This dataset has no description
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Mineral concentration in sediment core HU92045-11P
The continental slope in Orphan Basin, northeast of Newfoundland, is underlain by several seaward-thinning debris-flow wedges alternating with acoustically stratified,... -
Occurrence and type of dolomite in ODP Site 124-768 samples (Table 1)
Occurrence of deep-sea dolomites has been reported from numerous settings (for discussion see Lumsden, 1988). Different authors agree that dolomite formation in the pelagic... -
(Table 1) Peak intensities and stable carbon and oxygen isotope ratios of var...
Abundant and various diagenetic carbonates were recovered from a 1084-m-thick, Quaternary to lower Miocene section at ODP Site 799 in the Japan Sea. Petrographic, XRD, SEM,... -
(Tables 1-2) Composition of red coloured tills from Schobuell, Schleswig-Hols...
The stratigraphic position of the glacially transported 'Scholle' (large-size erratic block) at Schobüll near Husum (Schleswig-Holstein) is now considered to be Devonian rather... -
(Table T3) Calcium carbonate mineralogy of ODP Leg 182 sites, Great Australia...
Carbonate mineralogy was determined on a total of 2845 samples from Sites 1126-1132 situated on the southern margin of the Australian continent. Five of these sites represent... -
(Table T1) Calcium carbonate mineralogy and stable isotopic composition of OD...
Petrographic observation and carbonate mineralogic and stable isotopic investigation were conducted on lower Oligocene to middle Miocene sediments recovered during Ocean... -
(Table 1) Sediment composition, description and texture at DSDP Hole 93-603B
A 300-m-thick, upper Valanginian to Barremian turbidite sequence, consisting of sandstone and organic-matter-rich claystone turbidites intercalated in pelagic marl and... -
(Table 3) Textural and bulk mineralogy of Pliocene and Pleistocene sediments ...
The Pliocene and Pleistocene deposits recovered at Site 976 from the northwestern Alboran Sea at the Málaga base-of-slope include five main sedimentary facies: hemipelagic,... -
(Table 1) Mineralogy at DSDP Leg 81 Holes
This X-ray mineralogy study of Tertiary samples recovered from Rockall sites permitted the definition of four mineralogical units and the tracing of the paleoenvironmental... -
(Table 1) Mineralogy at DSDP Leg 79 Holes
Four sites in the region of the Mazagan Plateau off northwest Africa were drilled during Leg 79 of the Deep Sea Drilling Project. Bulk mineralogy and clay mineralogy were... -
(Table 1) Clay and non-clay mineral composition of dirty ice samples from acr...
Extensive dirty ice patches with up to 7 kg/m**2 sediment concentrations in layers of up to 10 cm thickness were encountered in 2005 and 2007 in numerous areas across the...