Correlating paleomagnetic, geochemical and petrographic evidence to date diagenetic and fluid flow events in the Mississippian Turner Valley Formation, Moose Field, Alberta, Canada

Author:

Cioppa M.T.,Al-Aasm I.S.,Symons D.T.A.,Lewchuk M.T.,Gillen K.P.

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference49 articles.

1. Al-Aasm, I.S., Lu, F., 1996. Multistage dolomitization of the Mississippian Turner Valley Formation, Quirk Creek Field, Alberta: chemical and petrologic evidence. In: Glass, D.J., Beauchamp, B., Embry, A.F. (Eds.), Pangea: Global Environments and Resources, Can. Soc. Pet. Geol. Memoir, vol. 17, pp. 657–675.

2. Stable isotope analysis of multiple carbonate samples using selective acid extraction;Al-Aasm;Chem. Geol. (Isot. Geosci. Sect.),1990

3. Al-Aasm, I.S., Lu, F., White, T., 1996. Evolution of pore fluids and dolomitization of Mississippian carbonates of Western Canada Sedimentary Basin: petrologic and chemical constraints, in: G.M. Ross (Compiler), Alberta Basement Transects Workshop, Lithoprobe Report #51, pp. 237–240.

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

5. Brine migration across North America—the plate tectonics of groundwater;Bethke;Ann. Rev. Earth Planet. Sci.,1990

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