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(Table 4) Geochemistry of groundmass titanomagnetites at DSDP Holes 82-557, 8...
Iron contents distributed as FeO and Fe2O3 according to R3O4 stoichiometry. -
(Table 3) Geochemistry of clinopyroxenes at DSDP Holes 82-557 and 82-561
This dataset has no description
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(Table 1) Trace element concentrations at DSDP Leg 82 Holes
This dataset has no description
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(Appendix A -Table 3) Geochemistry at DSDP Hole 82-559
Sediment depth is given in mbsf. All samples belong to Chemical Group I. -
(Appendix A -Table 1) Geochemistry at DSDP Holes 82-556 and 82-557
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(Table 11) Major and trace elements at DSDP Hole 82-559 basalts
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(Table 8) Major and trace elements at DSDP Hole 82-557 basalts
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(Table 5) Trace elements at DSDP Leg 82 Holes basalts
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(Table 3) Geochemistry of clinopyroxene and orthopyroxene at DSDP Holes 82-55...
This dataset has no description
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(Table 1) Geochemistry of plagioclase in DSDP Leg 82 Holes basalts
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(Table 3) Susceptibility anisotropy of plutonic rocks at DSDP Holes 82-556, 8...
This dataset has no description
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(Table 2) Intrinsic properties of plutonic rocks at DSDP Holes 82-556, 82-558...
This dataset has no description
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(Table 1) Remanent properties of plutonic rocks at DSDP Holes 82-556, 82-558 ...
This dataset has no description
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(Appendix B) Intrinsic properties of basalts at DSDP Leg 82 Holes
This dataset has no description
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(Appendix A) Remanent properties of basalts at DSDP Leg 82 Holes
This dataset has no description
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(Table A3) Bulk CO2 content for carbonates of ocean crust
Sediment depth is given in mbsf. Age represents the crustal age. -
(Table 1) Carbonate veins of DSDP and ODP holes
Age represents the crustal age. -
Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(Table 2) Geochemistry and petrograhy of DSDP Leg 82 Holes and MAPCO cruise o...
The compositions of abyssal glasses obtained on Leg 82 of the awGlomar Challenger and the MAPCO cruise of Jean Charcot have been investigated. Two main compositional groups of... -
Magnetic state of ocean basalts (Table 1)
The natural remanent magnetization (NRM) of ocean basalts, giving rise to the pattern of marine magnetic anomalies, is known to be of comparatively low intensity for about 20 Ma...