By A Mystery Man Writer
Download scientific diagram | dD vs. d 18 O plot displaying the isotopic compositions of smectite, smectite+illite, and kaolinite from the study area. The kaolinite lines indicate equilibrium with meteoric water at temperatures of 100ºC (Hayba et al., 1985). The supergene/hypogene line of kaolinite equilibrium with meteoric water at 35ºC is from Sheppard et al. (1969). The smectite line (SM) representing the isotopic composition in equilibrium with meteoric water at 20ºC is from Savin and Epstein (1970). The meteoric water line is from Craig (1961). from publication: COMPOSITION AND GENESIS OF THE NICKEL-CHROME-BEARING NONTRONITE AND MONTMORILLONITE IN LATERITIZED ULTRAMAFIC ROCKS IN THE MURATDAG˘ I REGION (US�AK, WESTERN ANATOLIA), TURKEY | Widespread lateritized ultramafic rocks in the southern part of the Muratdağı region of Turkey constitute a significant source of Ni-Cr-bearing ore with economic potential. However, no mineralogical or geochemical characterizations of these important materials have been | Chemical Weathering, Westerns and Hydrothermal | ResearchGate, the professional network for scientists.
Minerals, Free Full-Text
dD vs. d 18 O plot showing the isotopic compositions of smectites
Origin and modern microbial ecology of secondary mineral deposits
Smectite Group: Mineral information, data and localities.
Long-Term Stability of Bentonite - A Literature Review (pdf) - Posiva
Ancient origin of a rainforest in Gabon as revealed by carbon
Principles of sedimentology and stratigraphy [5. ed
The fossil record of igneous rock - ScienceDirect
Metal contamination in a sediment core from Osaka Bay during the
GeolCarp_Vol64_No1_23_38
GMGA – Grupo de Mineralogia e Geoquímica Aplicada – 03
Frontiers Origins of sediments and fluids in submarine mud
Distinct chemical and stable isotope compositions of smectite
Global Volcanism Program Bulletin of the Global Volcanism Network
Isotope Geochemistry of Oceanic Volcanics (Chapter 6) - Radiogenic