A NEW SYNTHESIS: CENTRAL TO SOUTHEASTERN ADIRONDACK MOUNTAINS, NEW YORK
The eastern part of the map area consists of a series of imbricate tectonic slices on ductile thrust zones and is called the SE allochthon. The SE allochthon is complex and is characterized by 10-15 times the volume of metagabbro intrusives relative to the shelf sequence, suggesting original proximity to an extensional axis. It also contains two (or more) major sills of the MCG series. An arcuate zone of biotite-quartz-plagioclase +/- potassium feldspar +/- sillimanite paragneisses along its western margin may represent a metamorphosed flysch deposit. Several exposures of granitic gneiss within the allochthon bear field evidence of almost complete anatexis of paragneisses.
The simplest history of the region involves early isoclinal and recumbent folding (F1) of the shelf sequence, followed by intrusion of the AMCG association, followed by open folding (F2) in the northern part of the map area becoming progressively tighter and overturned near the SE allochthon. An episode of ductile thrusting is roughly coeval with F2 folding. A final open folding (F3) with a N-S axial trend created an egg-carton pattern by interference with F2 folds.
The “Ticonderoga charnockite dome” appears to be an intrusive sheet that is domed by interference between F2 and F3 folds. The Springhill Pond and Thunderbolt Mountain metasedimentary/metavolcanic rocks mapped by Walton in the 1950’s appear to be another allochthon in the NE part of the map.