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(Table 5) R-mode factor scores of chemical component contents (on terrigenous...
This dataset has no description
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(Table 2) R-mode factor scores of chemical component contents in Mesozoic and...
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(Table 9) R-mode factor scores of chemical component contents in Mesozoic and...
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(Table 1) Composition of basalts from DEDP Leg 65 holes
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(Table 2) Major element composition of basalts from DSDP Leg 65 holes
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Electron Microprobe data for Hole BT1B Oman Drilling Project
Electron microprobe data for Serpentine, Spinel and carbonate (magnesite and dolomite) for 11 samples from Hole BT1B, Oman Drilling project. The discussion of the data is... -
Average compositions of serpentine and fuchsite from hole BT1B, Oman Drilling...
The presented serpentine and fuchsite (Cr-muscovite) data were derived from representative carbonate-bearing serpentinite and listvenite samples from Hole BT1B, OmanDP. Electron... -
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 S4. Past Himalayan erosion from Bengal Fan: Major and trace element res...
For the Bengal Fan samples, the measurements of major and trace elements were performed at SARM (Nancy, France), following (Carignan et al., 2001)... -
Summary of phase compositions of experimental silicate melt, un-normalised an...
The solubility of Re and Au in haplobasaltic melt has been investigated at 1673–2573 K, 0.1 MPa–2 GPa and IW-1 to +2.5, in both carbon-saturated and carbon-free systems. Results... -
(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 2) Petrophysical, petrological, and geochemical characteristics of ODP...
Ocean Drilling Program Hole 990A penetrated 131 m of subaerially emplaced Paleocene flood basalts on the Southeast Greenland margin with a recovery of 74%. Shipboard P-wave... -
(Table 1) Determined and theoretical chemical composition of thaumasite of OD...
Hole 841B was drilled in the forearc region of the Lau Basin at a water depth of 4810 m. The hole penetrated a roughly 500-m-thick series of Miocene volcanic sediments with a... -
(Table 2) Major and trace elements in the ash layer at DSDP Sample 95-613-34-...
A 2-5-cm-thick, middle to lower middle Eocene, vitreous ash layer of rhyolitic composition can be correlated between Sites 605 and 613 on the uppermost continental rise off New... -
(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... -
(Tables T1, T2) Major element content in alteration categories of ODP Site 19...
In the Ocean Drilling Program's only foray to an active seafloor hydrothermal system hosted by felsic volcanic rocks at a convergent plate margin, deep penetrations were... -
(Table T1) Major and trace element composition of sediment samples from ODP H...
Bulk geochemical analyses were carried out on 27 sediment samples located just above the igneous section of the incoming plate along the Costa Rican convergent margin. This... -
(Table T2) Major and trace element analysis of ODP Site 200-1224 basalts
During Ocean Drilling Program Leg 200, ~45 Ma igneous basement, was cored in the northeastern Pacific at Site 1224. The basement surface was inferred to be 28 meters below...