Optically continuous silcrete quartz cements of the St. Peter Sandstone: High precision oxygen isotope analysis by ion microprobe

Author:

Kelly Jacque L.,Fu Bin,Kita Noriko T.,Valley John W.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference71 articles.

1. Methodological improvements for investigating silcrete formation: petrography, Ft-IR and oxygen isotope ratio of silcrete quartz cement, Lake Eyre Basin (Australia);Alexandre;Chem. Geol.,2004

2. Arnold B. W., Bahr J. M. and Fantucci R. (1996) Paleohydrogeology of the Upper Mississippi Valley zinc–lead district. In Carbonate-hosted lead–zinc deposits. (ed. D. Sangster). Soc. Econ. Geol. 4, pp. 378–389.

3. Multiple overgrowths on detrital quartz sand grains in the Shakopee Formation (Lower Ordovician) of Minnesota;Austin;J. Sed. Petrol.,1974

4. Temperatures of mineral formation in bottom-run lead–zinc deposits of the Upper Mississippi Valley, as indicated by liquid inclusions;Bailey;Econ. Geol.,1951

5. Hydrologic constraints on the genesis of the Upper Mississippi Valley mineral district from Illinois Basin brines;Bethke;Econ. Geol.,1986

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