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Hinged Alleghanian Uplift of the Bronson Hill terrane in Connecticut and Massachusetts. Elizabeth R. Goeke, Julie L. Boyd, and Robert P. Wintsch Indiana University, Bloomington, Indiana. Research support by:.
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Hinged Alleghanian Uplift of the Bronson Hill terrane in Connecticut and Massachusetts Elizabeth R. Goeke, Julie L. Boyd, and Robert P. Wintsch Indiana University, Bloomington, Indiana
Research support by: • Geological Society of America Student Research grants awarded to Elizabeth R. Goeke and Julie L. Boyd • National Science Foundation grants #EAR 91-04495 (R. P. Wintsch) and #EAR99-09410 (R. P. Wintsch) • Department of Geological Sciences, Indiana University
Goals: To evaluate the Alleghanian overprint on rocks previously metamorphosed in the Acadian Orogeny.
Why the Bronson Hill terrane? • The entire terrane was metamorphosed during the Acadian Orogeny. • The terrane extends from the Long Island Sound to the New Hampshire/Canadian border. • Cooling ages from Connecticut in the Bronson Hill are indicative of cooling from Alleghanian events.
Ponder the Difference: • Hornblende ages are cooling from Alleghanian heating in the south and the Acadian Orogeny in the north. • Muscovite ages are fairly uniform the length of the terrane and indicative of cooling from Permian heating.
Thermometers and Barometers: • Holland and Blundy, 1994 hornblende-plagioclase thermometer • Graham and Powell, 1984 garnet-hornblende thermometer • Kohn and Spear, 1989 and 1990 garnet-hornblende-quartz-plagioclase barometer
Various P-T paths with gar-hb points, hb-pl points, and exhumation lines
Conclusions: • The southern portions of the Bronson Hill were buried to greater depths during the Alleghanian Orogeny than those in northern Connecticut and Massachusetts. • The Bronson Hill was exhumed quicker in the south than to the north.