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(Appendix 5) Major element composition of brucite, iowaite, chlorite and serp...
This dataset has no description
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(Appendix 5) Major element composition of hydrothermal amphibole in DSDP and ...
Sediment depth is given in mbsf. Cation numbers on the basis of 23 O. -
(Appendix 4) Average major element composition of spinel of serpentinized DSD...
Sediment depth is given in mbsf. Standard deviation relative to the average in %. Cation numbers on the basis of 4 O. -
(Appendix 4) Average major element composition of orthopyroxene of serpentini...
Sediment depth is given in mbsf. Standard deviation relative to average (raw composition data) or calculated error based on the Gaussian error propagation (cation numbers and... -
(Appendix 4) Average major element composition of olivine of serpentinized DS...
Sediment depth is given in mbsf. Standard deviation relative to average (raw composition data) or calculated error based on the Gaussian error propagation (cation numbers and... -
(Appendix 4) Average major element composition of clinopyroxene of serpentini...
Sediment depth is given in mbsf. Standard deviation relative to average (raw composition data) or calculated error based on the Gaussian error propagation (cation numbers and... -
(Table 1) Major element concentrations in abyssal peridotites from ODP Hole 2...
Data quality assessed using two rock standards (WS-E and OUG-94). Reproducibility is within 2% of recommended values with the exception of MnO, Na2O and P2O5 for WS-E which were... -
(Table 1, Appendix A2) Bulk rock composition of ODP Hole 209-1274A peridotites
The mode of peridotites was calculated by a mass-balance equation relating bulk rock and mineral compositions in the CFMAS system -
(Table 1, Appendix A2) Bulk rock composition of ODP Hole 209-1272A peridotites
The primary modal composition of peridotites was estimated from hand sample and thin section observations -
(Table 5) Analyses of representative tholeiites and tholeiitic ferrobasalts o...
This dataset has no description
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(Table 2) Major element analyses of representative Leg 91 basalts
CIPW norms calculated with assumed Fe2O3/Fe= ratio of 0.15. -
(Table 1) Chemical composition of hydrous and other minerals and their chromi...
This dataset has no description
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(Table 1) Chemical composition of hydrous and other minerals and their chromi...
This dataset has no description
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Major and trace element content of the 17 lithostratigraphic units recovered ...
IPOD Leg 49 recovered basalts from 9 holes at 7 sites along 3 transects across the Mid-Atlantic Ridge: 63°N (Reykjanes), 45°N and 36°N (FAMOUS area). This has provided further... -
Major and rare earth element concentrations of basalts beneath ODP Hole 118-7...
A wide-angle seismic experiment at the Atlantis II Fracture Zone, Southwest Indian Ridge, together with geochemical analyses of dredged basalt glass samples from a site... -
(Table 2) Mass balance calculations for ODP Hole 176-735B
Ocean Drilling Program Leg 176 deepened Hole 735B in gabbroic lower ocean crust by 1 km to 1.5 km. The section has the physical properties of seismic layer 3, and a total... -
(Table 1) Geochemistry of realatively fresh rocks of ODP Sites 127-794 and 12...
The flows and sills drilled at Sites 794 and 797 in the Yamato Basin of the Japan Sea are subalkalic, olivine, and/or plagioclase phyric basalts. Compositionally, the rocks can... -
(Table T1) Major and trace element concentrations of whole-rock samples from ...
Skiff Bank is a bathymetric and gravimetric high located ~350 km southwest of the Kerguelen Islands in the northern portion of the Kerguelen Igneous Province (KIP). Ocean... -
(Table T1) Geochemical composition of gabbroic rocks from ODP Hole 176-735B
Elemental data for 89 whole-rock samples from Hole 735B, 500-1500 meters below seafloor (Ocean Drilling Program Leg 176), are presented. The samples represent the rock types... -
(Table T1) Major element oxide and trace element concentration of ODP Hole 17...
Sixty-three major and trace element analyses from Hole 735B reflect known characteristics of the igneous and metamorphic evolution of the oceanic crust at this site. Regular...