Age and origin of the Boil Mountain ophiolite and Chain Lakes massif, Maine: implications for the Penobscottian orogeny

The Boil Mountain ophiolite complex of west-central Maine is widely interpreted to mark the Lower Ordovician Penobscottian suture between the Dunnage, Chain Lakes, and Gander terranes. The ophiolite consists of two distinct volcanic groups, including a lower island-arc tholeiite sequence and an uppe...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Kusky, T. M., Chow, J. S., Bowring, S. A.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1997
Subjects:
Online Access:http://dx.doi.org/10.1139/e17-051
http://www.nrcresearchpress.com/doi/pdf/10.1139/e17-051