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Abstract
The Precambrian geology of the Adirondack highlands was previously interpreted as a sedimentary terrane repeatedly invaded during the Grenville orogenic cycle by igneous intrusions to form successively the large anorthosite massif and satellites, numerous olivine gabbro and dolerite bodies, gneisses of the quartz-syenite and charnockite series, and granites. A reinterpretation is suggested.
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