dD vs. d 18 O plot displaying the isotopic compositions of smectite
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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.
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Stable isotope compositions (δ2H, δ18O and δ17O) of rainfall and
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PDF) Characterization of smectite to NH 4 -illite conversion
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dD vs. d 18 O plot displaying the isotopic compositions of
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Isotopes as tracers of magmatic sources
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Isotope Fractionation Processes of Selected Elements
![dD vs. d 18 O plot displaying the isotopic compositions of smectite](https://www.researchgate.net/profile/Selahattin-Kadir/publication/237971281/figure/fig1/AS:339630248480806@1457985569848/Simplified-general-stratigraphic-section-of-the-study-area-modified-from-Duru-et-al_Q320.jpg)
dD vs. d 18 O plots showing the isotopic compositions of the Sö g
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Volcanology and Geothermal Energy
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Frontiers Low-Temperature Clay Mineral Dehydration Contributes
![dD vs. d 18 O plot displaying the isotopic compositions of smectite](https://comptes-rendus.academie-sciences.fr/geoscience/article/CRGEOS_2012__344_11-12_704_0/jpg/src/tex/figures/gr1.jpg)
Processes controlling the stable isotope compositions of Li, B, Mg
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Microanalysis and mineralogy of Asian and Saharan dust
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Distinct chemical and stable isotope compositions of smectite
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Smectite Group: Mineral information, data and localities.
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