Geochemical evolution of peraluminous plutons in southern Nova Scotia, Canada—a pegmatite-poor suite

Author:

Currie K.L,Whalen J.B,Davis W.J,Longstaffe F.J,Cousens B.L

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference73 articles.

1. Internal structures in part of the South Mountain Batholith, Nova Scotia, Canada;Abbott;Geological Society of America Bulletin,1989

2. Pb and O isotopic constraints on the source of granitic rocks from Cape Breton Island, Nova Scotia, Canada;Ayuso;American Journal of Science,1996

3. Regional differences in lead isotopic compositions of feldspars from plutonic rocks of the northern Appalachian mountains, USA and Canada: a geophysical method of terrane correlation;Ayuso;Tectonophysics,1991

4. Genesis of the two main types of peraluminous granitoids;Barbarin;Geology,1996

5. Internally consistent thermodynamic data for minerals in the system Na2O–K2O–CaO–MgO–FeO–Fe2O3–Al2O3–SiO2TiO2–H2O–CO2;Berman;Journal of Petrology,1988

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