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(Table 4) Composition of pyroxenes from basalts the Bouvet triple junction
Sample types: 1, 4, 9, 11-13, 15 - clinopyroxene phenocrysts; 14 - clinopyroxene microphenocryst; 7, 8, 10, 16 - clinopyroxene microlites; 2, 3, 5, 6 - orthopyroxene phenocrysts. -
(Table 4) Major element analyses on pyroxenes of sediment core CRP-3
Structural formula recast on the basis of 4 cations and 6 oxygens -
(Table 2) Composition of selected pyroxene crystals in sediment core CRP-3
Atomic formula recalculated on the basis of 4 cations (6 O). -
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... -
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... -
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