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(Table 1) Mineralogy at DSDP Site 80-548
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(Table 1) Alteration mineralogy of ODP Hole 140-504B samples
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(Table 3) Mineral composition of ODP Site 161-975 sediments, Unit III
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(Table T5) Normative mineral composition of massive and semimassive sulfides ...
Curated sediment depth is given in mbsf. -
(Table T3) Normative mineral composition of ODP Hole 193-1189A and 193-1189B ...
Curated sediment depth is given in mbsf. -
(Table T1) Geochemistry of variably altered dacite from several ODP Leg 193 s...
Sediment depth is given in mbsf. Silicate d18O measurements were made on sulfate-free bulk rock powders. Where present, anhydrite was removed prior to analysis. For anhydrites,... -
(Table T2) Mineralogy of variably altered dacite from several ODP Leg 193 sites
Sediment depth is given in mbsf. Estimate of mineral abundance based on relative peak heights: ++ = dominant, + = common, (+) = rare, - not found. -
(Table 1) Mineral associations of ODP Hole 111-504B
= present, - = absent -
(Fig. 6) Distribution of detrital minerals, authigenic minerals, and biogenic...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent -
(Table 3) Distribution of detrital minerals, authigenic minerals, and biogeni...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent. Core 107-652A-36R Subunit IVb, 14 pebbles. -
(Table 3) Mineralogy of ODP Hole 107-652A
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(Table 2) Distribution of detrital minerals, authigenic minerals, and biogeni...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent -
(Table 1) Distribution of detrital minerals, authigenic minerals, and biogeni...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent -
(Table 28) Minerals from veins in basalts of the Costa Rica Rift
X - mixed-layer chlorite-montmorillonite mineral; X* - analysis of thomsonite has been obtained from N.N. Pertsev. -
(Fig. 7) Distribution of secondary minerals in basalts of the Costa Rica Rift...
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(Table 3) Mineralogy of selected hydrothermal precipitates from Mid Atlantic ...
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Abundance of minerals in the rocks of the upper peak ring from IODP Hole 364-...
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(Table T1) Physical properties of minicores from ODP Leg 193 sites, PACMANUS ...
Permeability of the ocean crust is one of the most crucial parameters for constraining submarine fluid flow systems. Active hydrothermal fields are dynamic areas where fluid... -
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... -
Smear slide analysis of Hole 64-477
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