-
(Table 8) Major-element compositions along profile across altered shard at DS...
All iron calculated as Fe2+. Empty cells indicates concentration below detection limit. -
(Table 7) Major-element compositions of selected secondary minerals: albite, ...
This dataset has no description
-
(Table 6) Major-element compositions of representative zeolites at DSDP Site ...
Empty cells indicates concentration below detection limit. All iron calculated at Fe2+. -
(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 3) Major-element compositions of representative clinopyroxenes at DSDP...
Fe3+ calculated assuming cation sum of 4.000. -
(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) Phillipsite and analcite chemical compositions at DSDP Leg 89 Holes
Cations/72 oxygens for phillipsites and cations/6 oxygens for analcites -
(Table 6) Celadonite chemical compositions at DSDP Leg 89 Holes
Cations/22 oxygens -
(Table 5) Smectite chemical compositions at DSDP Leg 89 Holes
Cations/22 oxygens -
(Table 4) Palagonite chemical compositions at DSDP Leg 89 Holes
This dataset has no description
-
(Table 3) Plagioclase chemical compositions at DSDP Leg 89 Holes
Cations/8 oxygens -
(Table T2) Major element oxides and atomic formulas of celadonite from ODP Ho...
Number of cations/oxygens, on which atomic formulas are based are given in the table. -
(Table T1) Major element oxides and atomic formulas of saponite from ODP Leg ...
Number of cations/oxygens, on which atomic formulas are based are given in the table. -
(Table 1) Chemical composition of minerals from IODP Hole 305-U1309D
Samples taken between 746.2 and 751.0 mbsf. -
(Table S6) Amphibole compositions of Pito Deep samples
Mineral formulas were recalculated on the basis of 23 anhydrous oxygens, using the 15 NK procedure of Robinson (1982). -
(Table S5) Chlorite and chlorite-smectite compositions of Pito Deep samples
This dataset has no description
-
(Table S3) Plagioclase compositions of Pito Deep samples
This dataset has no description
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(Table S7) Representative analyses of garnet from meta-chert samples VT08129 ...
Structural formulae have been calculated on the basis of 12 oxygens. #0 = below detection limit. -
(Table S5) Representative analyses of the epidote group minerals of sample VT...
Structural formulae have been calculated on the basis of 12.5 oxygens and 8 cations. All Fe assumed as Fe3+; Fe2+ calculated by charge balance to 25 negative charges. #0 = below...
