Geochemical constraints on the origin of secondary magnetizations in the Cambro-Ordovician Royer Dolomite, Arbuckle Mountains, southern Oklahoma

Author:

Elmore R.D.,Cates K.,Gao G.,Land L.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference37 articles.

1. Magnetic studies of the Pendleside Limestone: Evidence for remagnetization and late-diagenetic dolomitization during a post-Albian normal event;Addison;J. Geol. Soc.,1985

2. Brine migrations across North America — The plate tectonics of groundwater;Bethke;Annu. Rev. Earth Planet. Sci.,1990

3. Clay diagenesis in Wilcox Sandstones of southwest Texas: Implications of smectite diagenesis on sandstone cementation;Boles;J. Sediment. Petrol.,1979

4. Variation of seawater 87Sr86Sr through Phanerozoic time;Burke;Geology,1982

5. Thermal maturation by reflectance of Woodford Shale near Washita Valley Fault, Arbuckle Mountains, Oklahoma;Cardott,1990

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