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Heavy mineral composition of sediment core PM9499-2
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Heavy mineral composition of sediment core PM9462-4
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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) 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... -
(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... -
(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) Chemical composition of segregations and groundmass seperates of OD...
Concentrations of dark-colored, highly vesicular, quench-textured mesostasis occur commonly in volcanic rocks drilled in the Lau Basin during Leg 135. These segregations occur... -
(Table 1) Coarse-fraction (0.1 to 0.05 mm) mineralogy at DSDP Leg 55 Holes
This chapter was previously intended to trace volcanic episodes through the Neogene and Pleistocene geological history recorded in the sedimentary sections drilled on the... -
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... -
Abundance of minerals in the rocks of the lower peak ring from IODP Hole 364-...
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Heavy mineral composition of sediments of the West-Pakistan shelf (Table 4)
proportions of individual heavy mineral groups are determined by counting of circa 400 mineral grains -
Heavy mineral composition of alluvial sediments from southern West-Pakistan (...
proportions of individual heavy mineral groups are determined by counting of circa 400 mineral grains -
(App. 1) Distribution of the heavy minerals in sediment core DVDP-12
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(App. 3) Distribution of the heavy minerals in sediment core MSSTS-1
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(Table 1) Heavy mineral analysis of ODP Hole 151-913B
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(Appendix C) Heavy mineral composition of deep sea sediments in the Strait of...
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(Table 1) Modal mineralogy of basement rocks from ODP Hole 126-793B
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(Table 6) Modal mineralogy of basement rocks from ODP Hole 126-792E
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(Table 1) Heavy minerals in turbidites from DSDP Hole 19-183, the Aleutian ab...
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(Table 17) Mineral composition of heavy subfraction from rocks and sediments ...
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