Multiple fluid flow events and the formation of saddle dolomite: examples from Middle Devonian carbonates of the Western Canada Sedimentary Basin

Author:

Al-Aasm I,Lonnee J,Clarke J

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology

Reference6 articles.

1. Lonnee, J.S., Cioppa, M.T., Al-Aasm, I.S., Symons, D.T.A., Lewchuk, M.T., Gillen, K.P., 1998. Correlating paleomagnetic data with the paragenetic sequence in the Middle Devonian Sulphur Point Formation, northwestern Alberta. GAC-MAC-APGGQ Abstract Volume 23, A-112.

2. Low-flux, tectonically-induced squeegee fluid flowr (hot flash) into the Rocky Mountain Foreland Basin;Machel;Bull. Can. Petrol. Geol.,1999

3. Paleohydrogeology of the Canadian Rockies and origins of brines, Pb–Zn deposits and dolomitization in the Western Canada Sedimentary Basin;Nesbitt;Geology,1994

4. The Western Canada Sedimentary Basin;Porter;Trans. R. Soc. Lond.,1982

5. Introduction In: Western Canada Sedimentary Basin: a Case History;Ricketts;Can. Soc. Petrol. Geol.,1989

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