A possibility of 18O-depleted oceans in the Precambrian inferred from triple oxygen isotope of shales and oceanic crust
Yoshiki Kanzaki, Ilya N. Bindeman
Topics & Concepts
GeologyPrecambrianIsotopes of oxygenδ18OOceanic crustGeochemistryIsotope fractionationSedimentary rockCrustContinental crustMid-ocean ridgeStable isotope ratioEarth sciencePaleontologyBasaltSubductionTectonicsQuantum mechanicsPhysicsPaleontology and Stratigraphy of FossilsGeology and Paleoclimatology ResearchMethane Hydrates and Related Phenomena