ABSTRACT
Mispec Beach, New Brunswick is a coastal exposure of deformed Carboniferous
sedimentary rocks. Late Paleozoic deformation in the region is thought
to have occured in a restraining bend in the Cobiquid - Chedabucto fault.
Within this exposure, two main generations of deformation are recognized.
The first deformation is associated with slaty cleavage development, pebble
elongation, and the formation of quartz veins. The second generation structure
is a moderately developed crenulation cleavage. The diversity of structures
present at this outcrop allows for a qualitative determination of the principal
axes of stress and strain associated with the first generation structures.
Bradley, L.M., 1984. Structural analysis of deformed Carboniferous
strata, Mispec Beach, Southern New Brunswick. Unpublished MSc. thesis,
State University of New York at Albany. 134pp., +ix
University at Albany Science Library call number: SCIENCE Oversize
(*) QE 40 Z899 1984 B73
Return to MS Theses completed in the Geological
Sciences Program, University at Albany