Titlebook: Origin of Granite Batholiths Geochemical Evidence; Based on a meeting o M. P. Atherton,J. Tarney Book 1979 M.P. Atherton and J. Tarney 1979

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The Changing Pattern of Batholith Emplacement during Earth History,rozoic (e.g. Emslie, 1978). These two suites are chemically distinct and yet, in many cases, alkaline granites are sufficiently well developed to have been termed ‘batholithic’. They may, therefore, constitute an important contribution to past crustal growth. One of the two principal objectives of t

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s book. For reasons of length and cost, authors have been limited to presenting only the essential results necessary to develop their arguments and ideas. The comprehensive reference list will, however, assist those who wish to pursue specific aspects in greater detail. Inevitably, the cost and speed of publi978-1-4684-7990-4978-1-4684-0570-5

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M. P. Atherton,W. J. McCourt,L. M. Sanderson,W. P. Taylor

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An Emplacement Mechanism for Post-Tectonic Granites and Its Implications for Their Geochemical Featthe production of such zoning. To this end, the Ardara pluton, which has become one of the classic examples of a zoned post-tectonic pluton (Akaad, 1956), has been studied from a structural point of view.

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Compositional Variation in the Galloway Plutons,loway region assumes some geological importance in that all plate tectonic models of the Scottish Caledonian place one or more subduction zones near the present locations of the plutons (see review by Holland et al., in press).

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Transfusion