The hypothesis that increased stress on rocks induced during deformation produced microstructures on minerals, which gradually intensifies as one gets closer to an isograd line. This assumption is based on increasing microfractures in the fold...
The Rocky Hill anticline is a broad open fold in Triassic strata transverse to the
Eastern Border Fault of the Connecticut Valley of Southern New England, and is
crisscrossed by a complex pattern of faults and other brittle fractures. This study...
