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• W1988139464 endingPage "371" @default.
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• W1988139464 abstract "Composite acidic-basic dikes near Winnsboro, South Carolina, consist of cuspate pillow-like masses of basic rock surrounded by granite with no chilled margins or gradational boundaries. These dikes are similar to the net-veined complexes observed in other parts of the world. Most workers agree that these complexes represent coexisting acidic and basic liquids. Explanations of origin fall into two general classes: liquid immiscibility or commingling of miscible liquids. In the first, a homogeneous magma has unmixed to form two contrasting magmas. In the second, mixing was prevented because of high viscosities and rapid crystallization. The origin of these coexisting magmas in the second case has been variously explained by: coincidental intrusion of magma from different sources; melting of acidic rocks by the basic magma; or successive fractional melting of a common parent. These models are tested in the Winnsboro composite dike on the basis that the light REE's are partitioned in favor of the liquid in liquid-crystal equilibrium. In the Winnsboro dike, the light REE's are enriched in the basic rocks and relatively depleted in the granitic rocks. Thus, fractional crystallization of the basic rock or partial melting of the wall rock must be rejected." @default.
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• W1988139464 date "1978-05-01" @default.
• W1988139464 modified "2023-10-14" @default.
• W1988139464 title "Coexisting Acidic and Basic Melts: Geochemistry of a Composite Dike" @default.
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• W1988139464 doi "https://doi.org/10.1086/649696" @default.
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