FRACTURE PATTERNS, LINEAMENTS AND SEISMIC REFLECTION DATA: INTEGRATION FOR FAULT MAPPING IN THE APPALACHIAN BASIN OF EAST-CENTRAL NEW YORK STATE
Several characteristics of surface bedrock fractures were collected within the study area. Fracture characteristics include orientation, dip, spacing, fracture abutting relationships and fracture geometry. Fracture characteristics are displayed using modified rose diagrams to illustrate trends in orientation, frequency and fracture relationships. Three regional fracture orientations are common in the area: a NNE-striking joint set, an East-striking set, and a N60°E striking set. Fracture Intensification Domains (FIDs) are characterized by relatively closely spaced fractures; FIDs indicate areas where faulting is probable. Each of the three regional fracture orientations have zones of closely spaced fractures. FIDs recognized at the surface correlate spatially with thrust and high angle faults observed in 2-D seismic and with lineaments.
Lineaments identified from satellite imagery, digital elevation maps, and aeromagnetic gradients are combined with exposed bedrock fracture data and seismic reflection data. NNW-striking and NE-striking lineaments are coincident with aeromagnetic gradients in the field area. NNE-striking and N60ºE-striking lineaments are also coincident with fractures and FID orientations. The integration of these data promote mapping of FIDs in order to define areas with a higher probability of faults. This fault map will point to exploring areas that should be high-graded in the exploration for fracture-plays.