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(Table 1) Major element concentration of olivine from basalts of the West Val...
This dataset has no description
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(Table 3) Composition of the experimental phases and of minerals of gabbros f...
Glass analyses were normalized to anhydrous totals of 100 wt% to facilitate comparisons -
(Table 2) Chemistry of Fe-Ti-oxides from Pleistocene ash layers from ODP Hole...
This dataset has no description
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(Table 2) Chemistry of Fe-Ti-oxides from Pleistocene ash layers from ODP Hole...
This dataset has no description
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(Table 2) Chemistry of Amphibole from Pleistocene ash layers from ODP Hole 15...
This dataset has no description
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(Table 2) Chemistry of Clinopyroxene from Pleistocene ash layers from ODP Hol...
This dataset has no description
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(Table 2) Chemistry of Clinopyroxene from Pleistocene ash layers from ODP Hol...
This dataset has no description
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Microprobe analyses of opaque minerals in samples of the Admiralty Intrusive ...
This dataset has no description
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Microprobe analyses of opaque minerals in samples of the Admiralty Intrusive ...
This dataset has no description
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(Table 6) Major element analyses on amphibole found as isolated grains or int...
Structural fomula calculated on the basis of 23 cations -
(Table 4) Average composition of glass shards and glassy mesostasis in sedime...
This dataset has no description
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(Table 3) Representative chemical analyses of clinoamphibole and garnet in ba...
Structural formula calculated on the basis of 23 oxygens. -
(Table 4) Representative chemical analyses of hornblende and clinopyroxene in...
This dataset has no description
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(Table 3) Representative chemical analyses of biotite in basement clasts of s...
This dataset has no description
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Major element compositions of olivine, clinopyroxene and plagioclase, cooling...
As largest and best-exposed paleo-fast-spread oceanic crust on land, the Samail ophiolite in the Sultanate of Oman represents an ideal natural laboratory for investigating... -
(Table 1) Major and trace elements of basalts at DSDP Hole 72-516F
The geochemistry of basalts recovered during Leg 72 is described with emphasis on trace elements. Only Hole 516F penetrated basement; the basalts recovered are... -
(Table 1) Major and trace element composition of basalts from ODP Leg 163 sit...
During Leg 163, in the Southeast Greenland margin, drilling penetrated a thick succession of volcanic rocks that erupted during breakup of the North Atlantic in the early... -
(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... -
(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 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...
