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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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Heavy mineral analyses of sediment samples from the San Francisco Bay coastal...
Heavy or high-specific gravity minerals make up a small but diagnostic component of sediment that is well suited for determining the provenance and distribution of sediment... -
Heavy minerals of sediment core PS2792-5
percentages are recalculated on undetermined-free basis -
Heavy minerals of sediment core PS2719-1
percentages are recalculated on undetermined-free basis -
Heavy minerals of sediment core PL94-64
percentages are recalculated on undetermined-free basis -
Heavy minerals of sediment core PL94-60
percentages are recalculated on undetermined-free basis -
Heavy minerals of sediment core PL94-08
percentages are recalculated on undetermined-free basis -
Table 2. Selected electron microprobe analyses of mineral phases in the Eltan...
Analyses are in wt% and formula compositions in mol%. -
(Table 4) Major oxides in the dioritic pluton at DSDP Hole 66-493
Analysts are R. Duret and A. Pantaloni. -
(Table 1) Chemical compositions of clinopyroxene (and one glass matrix) in ba...
This dataset has no description
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(Table 4) Chemical composition of selected primary phases in ODP Hole 109-670...
This dataset has no description
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Composition of chromian diopside megacryst in DSDP Leg 37 basalts (Table 2, 3)
Refractory megacrysts of olivine, plagioclase, chromian diopside and Cr-Al spinel, which were not in equilibrium with the host oceanic tholeiite on eruption, are present in... -
(Table 1) Chemical composition and CIPW norms of basalts at DSDP Site 61-462
Analyst: H. Haramura. -
(Table 4) Chemical composition of pyroxene at DSDP Site 57-438
This dataset has no description
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(Table 3) Major-element chemistry of phases within flows, sills, and dikes fr...
Empty cells indicates that no analysis was made. -
(Table 1) Chemical compositions of boninite and basalt at DSDP Hole 60-458
Analyst: H. Haramura. Empty cells = no data. 1a and 3a are recalculated to 100% on an anhydrous basis. -
(Table 4) Geochemistry of glasses in boninite pillow fragments at DSDP Hole 6...
CIPW norms computed assuming Fe2+ /Fe2+ + Fe**3+ = 0.86. -
(Table 1) Geochemistry of gabbros at DSDP Hole 60-453
Empty cells = no data. CIPW norms are calculated assuming Fe2+ /Fe2+ + Fe**3+ = 0.86. -
(Table 2) Chemical composition and CIPW norms of glass at DSDP Hole 61-462A
Fe3+ / Fe2+ + Fe**3+ = 0.1. -
(Table 1) Basalt from DSDP Hole 66-487: Major elements and minerals
The CIPW norms are calculated with 85% of total iron as FeO and 15% as Fe2O3 (total Fe analysis is given as Fe2O3). Empty cells mean no data.