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Table D.14: Microprobe analyses of garnets from sample 2119
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.18: Microprobe analysis of garnets from samples no. 2168 and 2181
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.17: Microprobe analysis of garnets from sample no. 1563
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.15+16: Microprobe analysis of garnets from sample no. 1562
Number of ions on the basis of 24 O; oxides given in weight percentage -
Mineral chemistry data from batch experiments simulating hydrothermal troctol...
*Iron for andradite-grossular solid solutions was calculated as ferric Fe3+1Mg = Mg / (Mg + Fe) 2XCa = Ca / (Ca + Na) 3XFe = Fe / (Fe + Al) -
(Table 2) Partition coefficients for plagioclase of ODP Leg 135 vitrophyric r...
This dataset has no description
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(Table T2) Mean geochemistry and mineralogy of garnet sand grains from ODP Sa...
Sediment depth is given in mbsf. Number of ions is calculated on the basis of 12 oxygen atoms. Abundance of minerals is given in molecular percent, major element oxides in wt %. -
(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 1) Heavy minerals in silt and sand samples of IODP Site 301-U1301
The northwestern Cascadia Basin of western North America accumulated high-sedimentation-rate sequences during the Pleistocene sea-level low-stands. The continental shelf was...
