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(Table 5) Major element analyses on feldspar of sediment core CRP-3
Structural formula calculated on the basis of 8 oxygen atoms. -
Abundance of minerals in the rocks of the post impact formations from IODP Ho...
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Abundance of minerals in the rocks of the lower peak ring from IODP Hole 364-...
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Abundance of minerals in the rocks of the upper peak ring from IODP Hole 364-...
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Table 6 Generalised properties of Utsira caprocks, based on analysis of cutti...
Executive Summary: Carbon dioxide capture and storage (CCS) is one option for mitigating atmospheric emissions of carbon dioxide and thereby contributes in actions for... -
(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) Clay and non-clay mineral composition of dirty ice samples from acr...
Extensive dirty ice patches with up to 7 kg/m**2 sediment concentrations in layers of up to 10 cm thickness were encountered in 2005 and 2007 in numerous areas across the... -
(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... -
Mineralogy of nonclay components of Hole 325-M0058A
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(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... -
(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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(Table T2) Major element oxides and mineral composition of dolerites from ODP...
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Mineralogical analysis by X-Ray diffraction of Hashilan Wetland sediment core...
For mineralogical analysis by X-Ray Diffraction (XRD), samples of ~ 1 gram were dried at 50 °C for 48 hours. The dried samples were ground and homogenized using mortar and... -
XRD analyses of core Konar Sandal peat bog, SE Iran
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