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Related to Plutons: plutonic rock, batholith


An igneous intrusion.
A body of rock formed by metasomatic replacement.



the term used to signify deep-seated igneous bodies. Plutons form when magma from the lower part of the crust or from the mantle cools in the upper layers of the earth’s crust. Their various shapes are determined by the structure of the enclosing rock. Based on dimensions, shape, and bedding in the earth’s crust, the following types of plutons are distinguished: batholiths, laccoliths, lopoliths, phacoliths, dikes, and sills.

References in periodicals archive ?
Contrasting U-Pb ages from plutons in the Bras d'Or and Mira terranes of Cape Breton Island, Nova Scotia.
The focus of this study, the Landry Brook and Dickie Brook plutons anda group of smaller plutons, dykes, and sills referred to here as the Charlo plutonic suite, are part of this widespread mid-Paleozoic magmatism, but are spatially isolated from other plutonic manifestations of the magmatic event.
The age of the Saint George Plutonic Suite is broadly assigned to the Late Silurian to Late Devonian (New Brunswick Department of Natural Resources 2010), but the absolute ages of some of the constituent plutons are not well constrained.
The Wedgeport pluton in southernmost Nova Scotia differs in both age and composition from the abundant Devonian plutons that characterize the Meguma terrane (Fig.
Les plutons du CPM possedent generalement des caracteristiques chimiques calco-alcalines a intra-plaque, et leurs valeurs [[epsilon].
The Bras d'Or terrane of central Cape Breton Island is characterized by low- to high-grade metamorphic rocks intruded by abundant plutons of mainly Late Neoproterozoic age (Fig.
community activities Plutons located on Meroux common and Bourogne (90) by the Community of agglomeration Belfortaine project owner.
Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons.
The first systematic studies of the crustal structure of the pluton were carried out as part of deep seismic soundings (DSS) along International Profiles VI and VII within 1964-1972 using borehole shots (Beranek, 1971; Beranek et al.
These would have included the eight classical planets Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune, as well as the largest asteroid, Ceres, and a trio of outer--solar system objects termed plutons, including Pluto, its moon Charon, and Xena.
The other plutons are Charon and the newly found 2003 UB313.