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(Table 1) Mineral composition of clay fractions and bulk rocks, and δ¹⁸O, d2H...
Mineral contents are approximate -
(Table 1) Mineralogical assemblages of unaltered, altered and hydrothermal se...
x = very abundant, a = abundant, f = small quantity, * = allietit - talc-smectite mixed layer. -
Single-grain mineralogical data from two Antarctic ice cores (Dome B, Dome C)
Mineral species and polymorphs identified in two antarctic ice cores by single-grain Raman spectroscopy. Data are provided for the Holocene and for the last glacial period,... -
Abundance of minerals in the rocks of the upper peak ring from IODP Hole 364-...
This dataset has no description
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X-ray diffraction results from IODP Hole 357-M0076B
= 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-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-M0075A
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-M0071B
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-M0071A
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-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-M0068A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
(Table 1) Mineralogy of veins in basalts at DSDP Hole 61-462A
Numerous veins are present in basalts recovered from Hole 462A, Leg 61 of the Deep Sea Drilling Project. Three mineral assemblages are recognized and stratigraphically... -
(Table 1) Mineralogy of DSDP Leg 65 sediments
During Leg 65, four sites were drilled near the mouth of the Gulf of California where high sedimentation rates made it possible to sample young oceanic crust near the ridge... -
(Table 1) Bulk and clay mineralogy at DSDP Leg 66 Holes
During Leg 66 eight sites on an active margin transect off southern Mexico were drilled in order to determine the nature of ocean-continent transition across a subduction zone.... -
(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... -
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... -
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... -
Mineral composition of silt fraction from Hole 16-158
This dataset has no description
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(Table 4) Abundance of secondary minerals in basalts from the Northern and Ce...
This dataset has no description
