The geological water cycle and the evolution of marine δ 18 O values
- 1 August 2001
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 65 (15) , 2469-2485
- https://doi.org/10.1016/s0016-7037(01)00603-2
Abstract
No abstract availableKeywords
This publication has 71 references indexed in Scilit:
- Geologic evidence for a mantle superplume event at 1.9 GaGeochemistry, Geophysics, Geosystems, 2000
- 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawaterPublished by Elsevier ,1999
- The role of basalt weathering in the Sr isotope budget of the oceansPublished by Elsevier ,1999
- The Sr, C and O isotopic evolution of Neoproterozoic seawaterPublished by Elsevier ,1999
- Thermochemistry and phase equilibria of hydrous phases in the system MgO‐SiO2‐H2O: Implications for volatile transport to the mantleJournal of Geophysical Research, 1998
- Fluxes of mantle and subducted carbon along convergent plate boundariesGeophysical Research Letters, 1996
- Stability of hydrous phases in subducting oceanic crustEarth and Planetary Science Letters, 1996
- Methane‐rich fluids in the oceanic crustJournal of Geophysical Research, 1996
- The geochemical evolution of the continental crustReviews of Geophysics, 1995
- Fluids in accretionary prismsReviews of Geophysics, 1992