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(Table 9) Chemical composition of whole rocks from DSDP sites
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 1) Chemical composition of magnesian basalts and estimated primary magmas
This dataset has no description
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(Table 4) Chemical composition of basalts from ODP Hole 111-504B
This dataset has no description
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(Table 4) Chemical composition of surface sediments from the Transatlantic se...
Measurements of Eh have been carried out by A.V. Vershinin (SIO). CaCO3 and TOC contents have been measured by E.M. Zaslavsky (VNIRO), amorphous SiO2 and sulfur contents have... -
(Table T31) Chemical composition of basalts from Hole 332B, Leg 37 (FAMOUS ar...
This dataset has no description
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(Table 2) Major element composition of igneous rocks from DSDP Site 37-334
In samples marked by * the major element concentrations were determined by X-ray fluorescence; in other samples - by standard rapid methods at Dalhousie University. -
(Table 8) Geochemistry of DSDP Hole 65-485A basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
(Table 6) Geochemistry of DSDP Hole 65-483B basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
(Table 5) Geochemistry of DSDP Hole 65-483 basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
(Table 4) Geochemistry of DSDP Site 65-482 basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
(Table 2) Geochemistry of DSDP Hole 65-482B basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
Elemental geochemistry of the lower Pliensbachian Santiurde section (Basque-C...
We present inorganic elemental geochemistry from the lowermost Pliensbachian organic-rich hemipelagic Santiurde section (Basque-Cantabrian basin, north Iberian palaeomargin,... -
(Table 3) Chemical composition of glasses and middle and acid magmatic rocks ...
This dataset has no description
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Composition of chromian diopside megacryst in DSDP Leg 37 basalts (Table 2, 3)
Refractory megacrysts of olivine, plagioclase, chromian diopside and Cr-Al spinel, which were not in equilibrium with the host oceanic tholeiite on eruption, are present in... -
Major-element chemical analyses of Hole 37-335
This dataset has no description
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Major-element chemical analyses of Hole 37-333A
This dataset has no description
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Major-element chemical analyses of Hole 37-332B
This dataset has no description
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Major-element chemical analyses of Hole 37-332A
This dataset has no description
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Major-element chemical analyses of Hole 37-335
This dataset has no description
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Major-element chemical analyses of Hole 37-334
This dataset has no description