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(Table T6) Geochemical composition of Fe-Ti oxides from ODP Hole 176-735B gab...
This dataset has no description
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(Table T7) Geochemical composition of amphibole from ODP Hole 176-735B gabbros
This dataset has no description
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(Table T2) Major element oxides and cations of feldspar from ODP Hole 176-735...
Number of ions is calculated on the basis of 8 oxygen atoms. -
(Table T5) Major element oxides and cations of diopside from ODP Hole 176-735...
Number of ions is calculated on the basis of 6 oxygen atoms. -
(Table T6) Major element oxides and cations of mica from ODP Hole 176-735B veins
Number of ions is calculated on the basis of 22 oxygen (and OH) atoms. -
(Table T14) Major element oxides and cations of titanite from ODP Hole 176-73...
Number of ions is calculated on the basis of 4 Si atoms. -
(Table T13) Major element oxides and cations of apatite and zircon from ODP H...
Number of ions is calculated on the basis of 16 oxygen atoms. -
(Table T7) Major element oxides and cations of chlorite from ODP Hole 176-735...
Number of ions is calculated on the basis of 36 oxygen (and OH) atoms. -
(Table T15) Major element oxides and cations of clay minerals from ODP Hole 1...
Number of ions is calculated on the basis of 22 oxygen atoms. -
(Table T9) Major element oxides and cations of epidote from ODP Hole 176-735B...
Number of ions is calculated on the basis of 12.5 oxygen atoms. -
(Table T10) Major element oxides and cations of prehnite from ODP Hole 176-73...
Number of ions is calculated on the basis of 24 oxygen (and OH) atoms. -
(Table T11) Major element oxides and cations of ilmenite from ODP Hole 176-73...
Number of ions is calculated on the basis of 6 oxygen atoms. -
(Table T12) Major element oxides and cations of zeolite from ODP Hole 176-735...
Number of ions is calculated on the basis of 40 oxygen atoms. -
(Table 4) Analyses of titanomagnetic phenocrysts from ODP Hole 134-831B lavas
This dataset has no description
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(Table 1) Chemistry of plagioclases from ODP Holes 134-832B and 134-833B
Calculated on the basis of 8 O. -
(Table 2) Chemistry of olivine from ODP Holes 134-832B and 134-833B
Calculated on the basis of 4 O. -
(Table 3) Chemistry of pyroxene from ODP Holes 134-832B and 134-833B
Calculated on the basis of 6 O. -
(Table 4) Chemistry of Fe-Ti oxides from ODP Holes 134-832B and 134-833B
Calculated on the basis of 4 O. -
(Table 2) Chemistry of pyroxenes from ODP Leg 134 ash layers
Fe3+/Fe2+ calculated on the basis of charge balancing using Cameca propietary software. -
(Tables T3, T4) Major and trace element composition of fine-grained sediments...
Sediment depth is given in mbsf. The atomic formula for the hydrothermal chlorite has been calculated on the basis of the ideal O20(OH)16 anion content.
