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(Table 3) Chemical composition of single plagioclase from ODP Holes 104-642B ...
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(Table 3) Modal analyses of secondary minerals in weathered and hydrothermal ...
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(Table 4) Major and trace element content of basalts from DSDP Hole 49-409
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(Table 1ab) Chemical and mineral compositions of basalts from DSDP Hole 65-485A
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(Table 1ab) Chemical and mineral compositions of basalts from DSDP Hole 65-483B
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(Table 3) Major element composition of plagioclase phenocrysts from rock type...
Sample 125-786B-1R-1,88-92: Unit 1, bulk SiO2 = 62.48 wt.%. Sample 125-786B-51R-1,53-57: Unit 26, bulk SiO2 = 54.24 wt.% -
(Table 2) Major element composition of plagioclase phenocrysts from rock type...
Sample 125-786B-9R-1,25-30: Unit 3, bulk SiO2 = 56.43 wt.%. Sample 125-786B-15R-2: Unit 5, bulk SiO2 = 61.17 wt.%. -
(Table 2) Chemical composition of complexly zoned plagioclases from DSDP Hole...
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(Table 2) Chemical composition of complexly zoned plagioclases from DSDP Hole...
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(Table 2) Chemical composition of complexly zoned plagioclases from DSDP Hole...
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(Table 1) Chemical composition of simply zoned plagioclases from DSDP Site 45...
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Abundance of minerals in the rocks of the post impact formations from IODP Ho...
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(Table 1) Geochemistry of feldspars at DSDP Holes 62-464 and 62-465A
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 of K-feldspars and associated plagioclase phenocrysts ...
Basalts from some holes of the Deep Sea Drilling Project contain secondary K-feldspar which forms pseudomorphs after calcic (>76% An) Plagioclase cores, whereas Plagioclase... -
(Table 1) Oxygen and hydrogen isotope ratios of hydrothermal altered dolerite...
Dolerite samples, recovered in the dike complex between 1589 and 1991 meters below seafloor in Hole 504B during Legs 137/140, have been altered by hydrothermal fluids as shown... -
(Table 1) Mineral composition of ODP Hole 125-778A
The high-pressure, low-temperature metamorphic rocks known as blueschists have long been considered to form in subduction zones, where the descent of a relatively cold slab... -
Chemical analyses of ODP Hole 105-647A basalts (Table 2)
Basalt samples recovered from the lowermost 37 m of Leg 105 Hole 647A in the Labrador Sea are fine- to medium grained, have microphenocrysts of clinopyroxene, and show little... -
(Table 5, 6) Major and trace element content of basalts from DSDP Site 49-410
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(Table 1) Rock type and summary of alteration after component minerals in thi...
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Mineralogical composition of sediment core Sardarya from southeast Iran
The proxy data reported here are measured from a sediment core collected from Lake Sardarya (28° 38' 03" N, 61° 00' 44" E, 2675 m a.s.l.) situated on the western slope of Taftan...
