Petrogenesis of a silicic magma chamber periodically invaded by basaltic magma: The Isle au Haut Igneous Complex, Maine
The plutonic rocks of the Paleozoic Isle au Haut Igneous Complex, Maine (424 $\pm$ 1 Ma.), are a trimodal assemblage of granites, diorites, and gabbros. Exposed from the top to the bottom of the pluton, the complex consists of an enclave-bearing granite, a composite layered sequence of alternating g...
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Language: | ENG |
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ScholarWorks@UMass Amherst
1996
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Online Access: | https://scholarworks.umass.edu/dissertations/AAI9638940 |