Age and Regional Relationships of Granitoid Rocks of the Adirondack Highlands

Approximately 55% of the Adirondack highlands is underlain by granitic to tonalitic rocks that can be subdivided into five groups based on age, composition, and field occurrence: (1) early calcalkaline tonalites (ca. 1300 Ma) and associated granitic rocks (ca. 1250 Ma) of the southern and eastern hi...

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Veröffentlicht in:The Journal of geology 1991-07, Vol.99 (4), p.571-590
Hauptverfasser: Chiarenzelli, Jeffrey R., McLelland, James M.
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Sprache:eng
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