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Major element compositions in the upper peak ring from IODP Hole 364-M0077A
This dataset has no description
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Major elements, trace elements and Sr-Nd-Pb isotopes form lavas of lakes Nyos...
Lake Nyos is located at the summit of a stratovolcano in the Oku Volcanic Group (OVG) along the Cameroon Volcanic Line. The sudden release of magmatic CO2 trapped at the bottom... -
Table 5 to 12 - Concentration of major elements in samples from the Esmeralda...
Die vorliegende Arbeit besitzt mit der geologischen Kartierung des Marianen Trogs zwischen 15° und 18°N und der mineralogischen Untersuchung der hydrothermalen Gesteine im... -
Chemical compositions of representative lithologies from IODP Hole 357-M0076B
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0075B
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0072B
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0071C
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0071A
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0069A
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0068B
This dataset has no description
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Chemical compositions of representative lithologies from IODP Hole 357-M0068A
This dataset has no description
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(Supplement Table1) Abundances of major elements from KH93-3_DR10 at the Sout...
Petrographic and geochemical analyses of basaltic rocks dredged from the first segment of the Southwest Indian Ridge near the Rodriguez Triple Junction have been completed in... -
Geochemistry of free seep gases during Panarea shallow-water diving campaign
Location: Bottaro Crater, either within the diffusive seepage area (DSA) or at Vent C (VC). VC is one of the stronger vents at the west rim of the crater. -
(Table 2) Geochemistry of glasses at DSDP Leg 54 Holes, supplement to: Natlan...
The compositions of 45 natural basalt glasses from nine dredge stations and six Deep Sea Drilling Project Leg 54 sites near 9°N on the East Pacific Rise have been determined by... -
(Table 1) Geochemistry of sector-zoned crystal at DSDP Hole 45-395A, suppleme...
Variations in crystal morphologies in pillow basalts and probable sheet flows sampled from the region of the East Pacific Rise drilled during Leg 54 are related both to... -
(Table 1) Bulk geochemistry of some lavas at DSDP Hole 55-433C, supplement to...
According to Wilson's (1963a, b) hypothesis, the volcanoes of the Hawaiian-Emperor Chain are formed as the Pacific lithospheric plate moves over a source of magma in the mantle.... -
(Table 1) Chemistry of two samples of the red weathered layer at DSDP Hole 55...
One argument for the subaerial formation of Nintoku Seamount in the Emperor chain is the occurrence of a red claystone interlayered between two basalt flows in Hole 432A.... -
(Table 1) Geochemistry of ash layers at DSDP Leg 57 Holes, supplement to: Cad...
The study of the main characteristics of ash layers in Leg 57 cores shows that they are suitable for an analysis of the effect on eruptive activity of their distribution. We... -
(Table 1) Geochemistry of feldspars at DSDP Holes 62-464 and 62-465A, supplem...
Labradorite is the principal feldspar in tholeiitic basalt from Deep Sea Drilling Project Site 464, on northern Hess Rise. Andesine and oligoclase constitute most primary... -
(Table 2) Geochemistry at DSDP Holes 62-464 and 62-465A, supplement to: Seife...
Igneous rocks were recovered from three sites on Hess Rise during Deep Sea Drilling Project Leg 62: altered basalt at Site 464, at the northern end of Hess Rise; and altered...
