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(Table 1) Petrographical classification and mineral assemblage of basement cl...
This dataset has no description
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Modal analsyis of sediment core CRP-1 (Table 1)
This dataset has no description
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X-ray diffraction results from IODP Hole 381-M0080A
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
X-ray diffraction results from IODP Hole 381-M0079A
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
X-ray diffraction results from IODP Hole 381-M0078B
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
X-ray diffraction results from IODP Hole 381-M0078A
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
Environmental indicators in surface sediments of Lake Bolshoe Toko, Yakutia, ...
Here we present sedimentological, micro- and macropalaeontological, inorganic and organic geochemical, palaeomagnetic, and geochronological data as well as X-ray... -
Table 6 Generalised properties of Utsira caprocks, based on analysis of cutti...
Executive Summary: Carbon dioxide capture and storage (CCS) is one option for mitigating atmospheric emissions of carbon dioxide and thereby contributes in actions for... -
Mineral quantification of a Jordan Cretaceous outcrop (Section GM3, Ghawr Al ...
Cyclic fluctuations in global sea level during epochs of warm greenhouse climate have remained enigmatic, because absence or subordinate presence of polar ice during these... -
(Table 4) Mineralogy at DSDP Leg 55 Holes
On Leg 55, cores were takenfrom three seamounts in the Emperor Seamount chain: Ojin, Nintoku, and Suiko Seamounts. At the drilling sites the water depth was 1300 to 1700 meters;... -
(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... -
Mineralogical compositions of sediment samples from the San Francisco Bay coa...
The mineralogical compositions of 119 samples collected from throughout the San Francisco Bay coastal system, including bayfloor and seafloor, area beaches, cliff outcrops, and... -
(Table 2) Sorting and mineral composition of sediment obtained near Sylt, Nor...
Carefully selected sea bottom surface fine sand samples were studied from two sand ribbons normal to the shore. Possible sediment transport along these sand ribbons were... -
(Table T1) Mineral composition of turbidite sands and sandstones from ODP Leg...
During Ocean Drilling Program Leg 190 several turbidite successions in the Nankai Trough were drilled through including Pleistocene trench fill (Sites 1173 and 1174),... -
Fig. 2. Lithology, water and total carbon content, cumulative grain-size dist...
A 100 cm long sediment sequence was recovered from Beaver Lake in Amery Oasis, East Antarctica, using gravity and piston corers. Sedimentological and mineralogical analyses and... -
Composition of Carnian to Norian sandstones from the Wombat Plateau (Table 1)
The Carnian to Norian sediments, as much as 600 m in total thickness, recovered from ODP Sites 759 and 760 on the Wombat Plateau, are generally represented by fluvial-dominated... -
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,... -
Light mineral composition of 0.100-0.050 mm size fraction from Barents Sea se...
This dataset has no description
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Light mineral composition of 0.100-0.050 mm size fraction of sediments from C...
This dataset has no description
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Light mineral composition of 0.100-0.050 mm size fraction of sediments from H...
Method used - binocular counting
