Geochemical constraints on the origin of calcite veins and associated limestone alteration, Ordovician Viola Group, Arbuckle Mountains, Oklahoma, U.S.A.
- 1 August 1992
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 98 (3-4) , 257-269
- https://doi.org/10.1016/0009-2541(92)90188-b
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- U and Sr Isotopes in Ground Water and Calcite, Yucca Mountain, Nevada: Evidence Against Upwelling WaterScience, 1991
- North Sea chalk diagenesis: cementation of chalks and healing of fracturesChemical Geology, 1991
- Oxygen-isotope composition of diagenetic calcite in organic-rich rocks: Evidence for 18O depletion in marine anaerobic pore waterGeology, 1991
- Ages and stable-isotope compositions of secondary calcite and opal in drill cores from Tertiary volcanic rocks of the Yucca Mountain area, NevadaGSA Bulletin, 1990
- Sr isotope study of vein and cave calcites from southern IsraelChemical Geology, 1990
- Changes in marine isotopic composition and the late Ordovician glaciationJournal of the Geological Society, 1990
- Strontium isotopes as indicators of diagenetic recrystallization scales within carbonate rocksChemical Geology: Isotope Geoscience section, 1989
- Fluid flow in the crust; an example from a Pyrenean thrust rampAmerican Journal of Science, 1988
- Origin of calcite in syntectonic veins as determined from carbon-isotope ratiosGeology, 1983
- Stable isotopes and limestone lithificationJournal of the Geological Society, 1977