Low-temperature opal-CT precipitation in Antarctic deep-sea sediments: evidence from oxygen isotopes
- 31 December 1991
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 107 (3-4) , 612-617
- https://doi.org/10.1016/0012-821x(91)90105-q
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Chemical factors influencing the rates and sequences of silica phase transitions: Effects of organic constituentsGeochimica et Cosmochimica Acta, 1990
- A young porcellanite occurrence from the Southwest Indian RidgeMarine Geology, 1990
- Influence of rock composition on kinetics of silica phase changes in the Monterey Formation, Santa Barbara area, CaliforniaGeology, 1982
- Diagenetic trends in the siliceous facies of the Monterey Shale in the Santa Maria region, CaliforniaSedimentology, 1981
- A model for the origin of chert in limestoneGeology, 1979
- Diagenesis of late Cenozoic diatomaceous deposits and formation of the bottom simulating reflector in the southern Bering Sea*Sedimentology, 1978
- Oxygen isotope relations between diagenetic silica minerals in Monterey Shale, Temblor Range, CaliforniaAmerican Journal of Science, 1977
- Hydrogen and oxygen isotope ratios in nodular and bedded chertsGeochimica et Cosmochimica Acta, 1976
- Hydrogen and oxygen isotope ratios in silica from the JOIDES Deep Sea Drilling ProjectEarth and Planetary Science Letters, 1975
- New approach to surface seawater palaeotemperatures using 18O/16O ratios in silica of diatom frustulesNature, 1974