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Seismic reflection evidence for the evolution of a transcurrent fault system: The Norumbega fault zone, Maine

Geology (1996) 24 (3): 251–254.
This article has been cited by the following articles in journals that are participating in CrossRef Cited-by Linking.
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Coupling of deformation and reactions during mid‐crustal shear zone development: an in situ frictional–viscous transition
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Assessing the role of orogen-parallel faulting in post-orogenic exhumation: low-temperature thermochronology across the Norumbega Fault System, Maine
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Late Cretaceous reactivation of the Norumbega fault zone, Maine: Evidence from apatite fission-track ages
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Sequential ductile to brittle reactivation of major fault zones along the accretionary margin of Gondwana in Central Argentina
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Lithospheric evolution in the wake of the Mendocino triple junction: structure of the San Andreas Fault system at 2 Ma
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Evolution of a transcurrent fault system in shallow crustal metasedimentary rocks: the Norumbega fault zone, eastern Maine
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