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X-ray diffraction mineralogy of sediment core MD99-2323
Weight % of non-clay and clay minerals based on quantitative X-ray diffraction using the “whole-pattern” Rockjock v6.0 Excel macro program (calibrated with 10% zincite) (Eberl,... -
Microwave-induced self-organization in mineral systems. V. FeCl3 colloid (800...
Microwave-induced self-organization in FeCl3 colloids under high irradiation power (800 W) is strongly dependent on the layer thickness of the precursor (saturated ferric... -
Microwave-induced self-organization in mineral systems. IV. FeCl3 colloid (45...
Membraneous structure self-organization in FeCl3 colloids under microwave treatmet (450 W, 2.45 GHz) occurs due to the hydrolytic polycondensation of the ferric oxohydroxides. A... -
Microwave-induced self-organization in mineral systems. III. FeCl3 colloid (2...
Microwave-induced self-organization of membraneous structures with different morphology in hydrolized FeCl3 colloid (200 W, 2.45 GHz,1 min). The local MW treatment conditions... -
(Table 1) Mineralogical composition of sediments from DSDP Sites 69-504 and 6...
We discuss the provenance of minerals detected by X-ray-diffraction analyses of sediments of Sites 504 and 505 of Deep Sea Drilling Project Leg 69. These are X-ray-amorphous... -
(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... -
XRD mineralogy of sediments from the Greenland east coast
Quantitative X-Ray Diffraction (qXRD) analysis of the <2 mm sediment fraction from surface (sea floor) samples, and marine sediment cores that span the last 10-12 cal ka BP,...