-
X-ray diffraction analysis of sediments of IODP Hole 302-M0002A
Results of X-ray diffraction analysis and quantification of mineral phases based on the full-pattern method QUAX (Vogt, C., Lauterjung, J. and Fischer, R.X., 2002. Investigation... -
(Table 1) Measured and reconstructed primary modes of peridotites from ODP Ho...
Measured modes based on 1000 point per thin section (1215 points for 109-670A-9R-1,94-97). Grid spacing = 0.5 mm. <1 = traces. -
(Table 1) Modal analyses of selected samples of ODP Hole 109-670A
This dataset has no description
-
(Table 1) Minerals of ODP Hole 103-637A peridotites
= present, - = absent -
(Table 1) Heavy minerals in turbidites from DSDP Hole 19-183, the Aleutian ab...
This dataset has no description
-
(Table 6) Modal mineralogy of basement rocks from ODP Hole 126-792E
This dataset has no description
-
(Table 1) Modal mineralogy of basement rocks from ODP Hole 126-793B
This dataset has no description
-
(Table 1) Heavy mineral analysis of ODP Hole 151-913B
This dataset has no description
-
(Table 1, Appendix A2) Bulk rock composition of ODP Hole 209-1274A peridotites
The mode of peridotites was calculated by a mass-balance equation relating bulk rock and mineral compositions in the CFMAS system -
(Table 1, Appendix A2) Bulk rock composition of ODP Hole 209-1272A peridotites
The primary modal composition of peridotites was estimated from hand sample and thin section observations -
(Table 4) Reconstructed primary mineralogy, composition, and mass change duri...
For the modal data, 1000 points have been counted in the thin sections on a 0.2x0.2 mm grid. The modal data are given in vol. %. Modal proportions of primary minerals are given... -
(Table 2) Reconstructed primary modal compositions of representative ODP Hole...
Sample composition is represented by a single, standard-sized, thin section (~6,000 points). Composition is given in vol % -
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... -
(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... -
(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) 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) 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... -
X-ray diffraction analysis of sediments from ODP Hole 178-1095B
This dataset has no description
-
Smear slide investigation on ODP Hole 202-1242A
This dataset has no description
