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(Table 1) Distribution of smectite and silica in sediments adjacent to and wi...
Total peak areas of 17-, 10-, and 7-A clay minerals are shown. Typical detrital terrigenous clay from North Pacific - Bering Sea area is about 80 to 125 cm**2. This parameter... -
(Table 1) Distribution of smectite and silica in sediments adjacent to and wi...
Total peak areas of 17-, 10-, and 7-A clay minerals are shown. Typical detrital terrigenous clay from North Pacific - Bering Sea area is about 80 to 125 cm**2. This parameter... -
(Table DR1) Silicic tephras at ODP Sites 162-983 and 162-984
This dataset has no description
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(Table DR1) Silicic tephras at ODP Site 152-919
This dataset has no description
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(Table DR1) Silicic tephras in ODP Hole 162-985B
This dataset has no description
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(Table DR1) Silicic tephras in ODP Hole 162-985A
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(Table DR1) Silicic tephras in ODP Hole 162-907B
This dataset has no description
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(Table DR1) Silicic tephras in ODP Hole 151-907A
This dataset has no description
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(Table 1) Proportions of clay minerals and mud, as well as description of sed...
The clay mineralogy of Lower Cretaceous deep-sea fan sediment in the western North Atlantic is dominated by smectite in most intervals, and by illite in samples from intervals... -
(Table T1) Olivine-gabbro sequence description of ODP Hole 118-735B
Olivine gabbros, allied troctolitic gabbros, and troctolites, together making up the olivine gabbro suite, comprise some 76% of the section cored in Hole 735B on the eastern... -
(Table 1) Composition of selected ash layers in ODP Site 126-792
Glass shards from 26 megascopic tephras (1-29 cm thick) were separated and analyzed for 26 elements and 87Sr/86Sr and 143Nd/144Nd isotope ratios. The isotope data allowed us to... -
Wet-bulk density and mean silt diameter gradients for density anomaly interva...
Terrigenous sediments between 800 and 1147 mbsf at Site 645 in Baffin Bay display intervals tens of centimeters thick, in which wet-bulk density either rapidly increases or... -
Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1)
Native Cu occurs in amygdules, fractures and groundmass of tholeiites from Ocean Drilling Program Site 642 on the Vøring Plateau. Similar occurrences have been reported in other... -
(Table DR1) Biogenic silica and chert in the Pacific Ocean, DSDP and ODP data
Evidence for the dissolution of biogenic silica at the base of pelagic sections supports the hypothesis that much of the chert formed in the Pacific derives from the dissolution... -
(Table 2) Mass balance calculations for ODP Hole 176-735B
Ocean Drilling Program Leg 176 deepened Hole 735B in gabbroic lower ocean crust by 1 km to 1.5 km. The section has the physical properties of seismic layer 3, and a total... -
(Table A1) Bottom layer properties during Nathanial B. Palmer cruise NBP00-08...
Dissolved oxygen was originally given in ml/l and was recalculated to µmol/l by multiplying by 44.66; Definition of concentration at bottom and accross bottom layer thickness... -
(Table A2) Bottom layer properties during Nathanial B. Palmer cruise NBP04-08...
Dissolved oxygen was originally given in ml/l and was recalculated to µmol/l by multiplying by 44.66; Definition of concentration at bottom and accross bottom layer thickness... -
(Table 2) Positions of the redox line and the ratio of the thickness of the o...
Sediment temperatures are given in Table 1, see: -
Thickness of sea ice during POLARSTERN cruise ANT-XXIII/7 (Winter Weddell Out...
This dataset has no description
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Microfossils in surface sediments of brackish waters from the South African w...
A faunistic survey covering 25 sites in estuaries, coastal lakes and ponds along the west coast of South Africa between the Cape of Good Hope in the south and the Olifants River...
