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.
dD vs. d 18 O plot showing the isotopic compositions of smectites
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dD vs. d 18 O plot displaying the isotopic compositions of
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