-
(Table 3) Representative olivine compositions of ODP sample 140-504B-222R-1,0...
Cations calculated on the basis of 4 oxygens. -
(Table 3) Cr-rich spinel geochemistry of DSDP Hole 38-338 and ODP Hole 152-917A
This dataset has no description
-
(Table 2) Representative Cr-rich spinel geochemistry of DSDP Hole 38-338 and ...
This dataset has no description
-
(Table 9) Geochemistry of alteration minerals at DSDP Hole 83-504B
This dataset has no description
-
(Table 3) Major element oxides and mineral composition of samples from ODP Le...
This dataset has no description
-
(Table 4) Geochemical composition of experimental olivine from ODP Holes 152-...
This dataset has no description
-
(Table 4) Geochemistry of titanaugite from basalt at DSDP Hole 84-567A
Empty cells indicate no detection or trace. -
(Table 3) Geochemistry of zeolite at DSDP Hole 84-567A
Empty cells indicate no detection or trace. -
(Table 2) Geochemistry of metallic sediments at DSDP Hole 84-567A
Empty cells indicate no detection or trace. -
(Table 7) Geochemistry of spinels at DSDP Leg 84 Holes
Elements as atoms per 32 oxygens. Small denotes analyses of grains on same order of size as spot (generally less than 30 µm); core and rim denote, respectively, analyses of the... -
(Table 6) Geochemisty of clinopyroxene at DSDP Leg 84 Holes
Elements as atoms per 6 oxygens. -
(Table 5) Geochemistry of orthopyroxene at DSDP Leg 84 Holes
Elements as atoms per 6 oxygens. -
(Table 4) Geochemistry of olivine at DSDP Holes 84-567A and 84-566C
Elements as atoms per 4 oxygens. -
(Table 3) Geochemistry of serpentinites at DSDP Leg 84
This dataset has no description
-
(Table 2) Olivines from ultramafic rocks at DSDP Hole 84-567A and Site 84-566
Formula basis: 4 oxygens. -
(Table 2) Chemical composition of pyroxene from DSDP Hole 89-462A
This dataset has no description
-
(Table 5) Major-element compositions of sheet silicates at DSDP Site 89-585
<0 = concentration below detection limit. Total iron calculated as Fe2+. -
(Table 4) Major-element compositions of palagonite-type altered glass shards ...
All iron calculated as Fe2+. <0 = concentration below detection. -
(Table 2) Major-element compositions of selected primary minerals: plagioclas...
Empty cells indicates concentration below detection limit. All iron in feldspar calculated as Fe3+, as Fe2+ in kaersutite and biotite; Fe3+ in oxides calculated assuming cation... -
(Table 7) Geochemistry of olivine from ODP Leg 135 holes lavas
This dataset has no description
