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X-ray diffraction results from IODP Hole 357-M0075B
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0072B
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0071C
= poor data quality. Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized... -
X-ray diffraction results from IODP Hole 357-M0069A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0068B
= poor data quality, ** = duplicate sample. Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or... -
X-ray diffraction results from IODP Hole 357-M0068A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
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 1) Percentage of non-opaque heavy minerals, heavy residue, magnetite, ...
Heavy-mineral analyses were made for 39 samples, 27 from DSDP Site 445 and 12 from Site 446. About one-fourth of the samples were so loose that they were easily disaggregated in... -
(Table 1) Mineralogical composition of sediments from DSDP Sites 69-504 and 6...
We discuss the provenance of minerals detected by X-ray-diffraction analyses of sediments of Sites 504 and 505 of Deep Sea Drilling Project Leg 69. These are X-ray-amorphous... -
(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... -
(Table 1) Oxygen and hydrogen isotope ratios of hydrothermal altered dolerite...
Dolerite samples, recovered in the dike complex between 1589 and 1991 meters below seafloor in Hole 504B during Legs 137/140, have been altered by hydrothermal fluids as shown... -
Heavy mineral analyses of sediment samples from the San Francisco Bay coastal...
Heavy or high-specific gravity minerals make up a small but diagnostic component of sediment that is well suited for determining the provenance and distribution of sediment... -
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 1) Mineral composition of 0.100-0.050 mm size fraction from surface la...
Distribution of mineral assemblages in sediments of both shelf and continental slope of Vietnam is under consideration. Mineral provinces are recognized and their... -
(Table 1) Framework-grain composition of ODP Leg 125 sediment samples
This report presents petrographic data that will be used to characterize spatial and temporal changes in the provenance of Izu-Bonin forearc sediments recovered during Ocean... -
(Table 1) Heavy mineral content in sediments of the southern Mediterranean Ri...
Petrographic analysis of Quaternary terrigenous sand layers in eastern Mediterranean cores reveals distinct mineralogical differences between the Egyptian Shelf–Nile Cone region... -
Schwermineraltabelle
Die Altersbestimmung von Sedimentärgeschieben, die nicht durch ihren Fossilgehalt hinreichend gekennzeichnet sind, ist nur auf dem Wege eines petrographischen Vergleiches mit... -
(Table 1) Heavy minerals in silt and sand samples of IODP Site 301-U1301
The northwestern Cascadia Basin of western North America accumulated high-sedimentation-rate sequences during the Pleistocene sea-level low-stands. The continental shelf was... -
Mineralogy of serpentine muds of ODP Leg 125 holes (Table 1)
Large serpentinite seamounts are common in the forearc regions between the trench axis and the active volcanic fronts of the Mariana and Izu-Bonin intraoceanic arcs. The... -
Heavy mineral content of ODP Leg 107 holes
Analyses of rock clasts and of heavy minerals in upper Miocene coarse detrital units drilled along the East Sardinia passive-type continental margin (Sites 654, 653, 652, and...
