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(eTable 1) Geochemistry of plagioclase traverses, ODP Hole 106-648B and 109-648B
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(Table 1) Anorthite and Sr contents of plagioclase tracerses
Anorthite in mol%. -
(Table 3) Hysteresis parameters and ratios Rh and Rj of core samples of ODP H...
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(Table 2) Susceptibility and anisotropy of the susceptibility of core samples...
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(Table 1) Petrography, Curie temperature and magnetic concentration of core s...
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(Table 3) Chemistry of basalts from ODP Hole 109-648B
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(Table 2) Hysteresis loop parameters and Curie temperatures in ODP Hole 109-648B
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(Table 1) Magnetic remanent properties for ODP Hole 109-648B
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(Table 2) Magnetic parameters and Curie temperature of samples from ODP Hole ...
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(Table 1) Magnetic fabrics in ODP Hole 109-670A
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(Table 4) Mineral chemistry of peridotites from ODP Hole 109-670A
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(Table 3) Oxygen isotopes in serpentine from ODP Hole 109-670A
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(Table 2) Grain sizes of minerals from ODP Hole 109-670A
Estimates of pre-serpentinization dimensions based on measurements of primary grains and pseudomorphs. -
(Table 1) Measured and reconstructed primary modes of peridotites from ODP Ho...
Measured modes based on 1000 point per thin section (1215 points for 109-670A-9R-1,94-97). Grid spacing = 0.5 mm. <1 = traces. -
(Table 2) Groundmass plagioclase size in lavas from Serocki volcano sampled i...
Plagioclase width is the average of 6-12 of the largest crystals in each thin section measured perpendicular to the (010) crystal faces. -
(Table 2) TRM acqusition test for some samples having negative inclinations, ...
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(Table 1) Paleomagnetic data of basalts from ODP Hole 109-648B
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(Table 2) Inclinations and declination differences of oriented samples of ODP...
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(Table 1) NRM intensity, MDF, susceptibility and Q-ratio of serpentinized per...
This dataset has no description
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(Table 2) Whole-rock oxygen isotope geochemistry of serpentinized peridotites...
This dataset has no description