Magmatic changes during the stabilisation of a cordilleran fold belt: the Late Carboniferous–Triassic igneous history of eastern New South Wales, Australia

Author:

Caprarelli Graziella,Leitch Evan C.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference63 articles.

1. Albarède, F., 1995. Introduction to Geochemical Modelling. Cambridge Univ. Press, Cambridge.

2. Ashley, P.M., Cook, N.D.J., Hill, R.L., Kent, A.J.R., 1993. Lamprophyre dykes and their relation to mesothermal Au–Sb veins at Hillgrove, southern New England Orogen, New South Wales. In: Flood, P.G., Aitchison, J.C. (Eds.), New England Orogen, Eastern Australia. Department of Geology and Geophysics, University of New England, Armidale, NSW, Australia, pp. 359–375.

3. Asthana, D., 1984. Intermediate, mafic and ultramafic rocks from the eastern part of the New England Fold Belt: chemistry, relict mineralogy, magmatic affinities and tectonic significance. PhD thesis, University of Sydney, Sydney, Australia.

4. Petroi Metabasalt: alkaline within-plate mafic rocks from the Nambucca Slate Belt, northeastern New South Wales;Asthana;Australian Journal of Earth Sciences,1985

5. Petrogenesis of Hercynian leucogranites from the southern Armorican Massif: contribution of REE and isotopic (Sr, Nd, Pb and O) geochemical data to the study of source rock characteristics and ages;Bernard-Griffiths;Earth and Planetary Science Letters,1985

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