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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. -
(App. 3) Distribution of the heavy minerals in sediment core MSSTS-1
This dataset has no description
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Abundance of minerals in the rocks of the lower peak ring from IODP Hole 364-...
This dataset has no description
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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-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. -
(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) 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... -
(Table 1) Rock type and summary of alteration after component minerals in thi...
This dataset has no description