Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Metamorphism in the Potomac composite terrane, Virginia-Maryland

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6875987
Metamorphic rocks in the Potomac Valley occur in three allochthon-precursory melange pairs unconformably overlain by the Popes Head Formation which is at greenschist facies of metamorphism. The highest motif, the Piney Branch Complex and Yorkshire Formation are also in the greenschist facies. The middle motif, consists of the Peters Creek Schist and the Sykesville Formation. Quartzose schists and metagraywacke of the Peters Creek contain serpentinite debris and have had a complex metamorphic history: Barrovian prograde to amphibolite facies (with sillimanite), a localized retrograde event producing chlorite phyllonite, and a later greenschist prograde event. The Sykeville is at biotite +/- garnet grade and contains deformed olistoliths of Peters Creek, including phyllonite, at various grades. The lower motif consists of the Annandale Group (pelitic schists and metasandstone) and Indian Run Formation. The Annandale has experienced two greenschist metamorphisms. The Indian Run is at biotite +/- garnet grade and contains previously metamorphosed and deformed olistoliths of Annandale. The allochthons have had different histories, but after stacking they were metamorphosed with their melanges and the Popes Head to biotite grade. The Popes Head has experienced three phases of folding, the earliest synkinematic with Occoquan emplacement. These fold phases are superposed on earlier structures in the older rocks and are probably of Late Cambrian age (Penobscotian). Earlier deformation is probably of Late Proterozoic age (Cadomian). Neither of these deformations is recognized in North American rocks.
Research Organization:
Geological Survey, Reston, VA (USA)
OSTI ID:
6875987
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
Country of Publication:
United States
Language:
English

Similar Records

Penobscot and Taconic events in the central Appalachian Piedmont, northern Virginia-Maryland
Conference · Mon Feb 28 23:00:00 EST 1994 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:6888057

Quantitative estimates of metamorphic equilibria: Tallassee synform, Dadeville belt, Alabama's Inner Piedmont
Conference · Sun Feb 28 23:00:00 EST 1993 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:5951225

Low-angle normal faults in the south-central Brooks Range fold and thrust belt, Alaska
Journal Article · Sun May 01 00:00:00 EDT 1988 · Geology; (United States) · OSTI ID:6991195