Sedimentary melanges of the central Appalachian
Conference
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6644686
Crystalline thrust sheets in the central Appalachian Piedmont typically overlie precursory sedimentary melanges forming tectonic motifs. The melanges have quartzofeldspathic matrices, contain an assortment of exotic olistoliths including ultramafic rocks, and each is characterized by a debris of the immediately overlying thrust sheet. The olistoliths are foliated, many are polydeformed, and were polymetamorphosed before the inclusion in the matrix. Subsequently the melange was metamorphosed and deformed again. Olistoliths are rectilinear to lensoid range from small chips to blocks as long as 1.5 km, and lie parallel with the matrix foliation. These melanges have been recognized from Trenton, New Jersey, to northern Virginia, on all sides of the hypothetical Baltimore Gneiss microcontinent, a probably window, and serve as markers for individual thrust sheets. The melanges seem to be large subaqueous slide deposits that were triggered by the advancing thrust sheets that now overlie them. Similar modern deposits occur on trench slopes where this is sufficient sediment for their construction. With continuing deformation, the debris was overrun by the thrust sheet forming a motif. The process continued until deformation ceased resulting in a stack of motifs. The rocks have a mixture of deformational fabrics resulting from both gravitational and tectonic processes, but the boundary between each melange and its overlying thrust sheet is tectonic, commonly a retrograded shear zones.
- Research Organization:
- Geological Survey, Reston, VA (USA)
- OSTI ID:
- 6644686
- 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
Liberty Complex: polygenetic melange in the central Maryland Piedmont
Penobscot and Taconic events in the central Appalachian Piedmont, northern Virginia-Maryland
Metamorphosed melange in the central Piedmont of South Carolina
Conference
·
Mon Dec 31 23:00:00 EST 1984
· Geol. Soc. Am., Abstr. Programs; (United States)
·
OSTI ID:6453918
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
Metamorphosed melange in the central Piedmont of South Carolina
Journal Article
·
Fri Sep 01 00:00:00 EDT 1989
· Journal of Geology; (USA)
·
OSTI ID:7135907
Related Subjects
58 GEOSCIENCES
580201* -- Geophysics-- Seismology & Tectonics-- (1980-1989)
580300 -- Mineralogy
Petrology
& Rock Mechanics-- (-1989)
DEFORMATION
FEDERAL REGION II
FEDERAL REGION III
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC MODELS
GEOLOGIC STRATA
GEOLOGIC STRUCTURES
GEOLOGY
LITHOLOGY
METAMORPHIC ROCKS
NEW JERSEY
NORTH AMERICA
PETROLOGY
ROCKS
TECTONICS
USA
VIRGINIA
580201* -- Geophysics-- Seismology & Tectonics-- (1980-1989)
580300 -- Mineralogy
Petrology
& Rock Mechanics-- (-1989)
DEFORMATION
FEDERAL REGION II
FEDERAL REGION III
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC MODELS
GEOLOGIC STRATA
GEOLOGIC STRUCTURES
GEOLOGY
LITHOLOGY
METAMORPHIC ROCKS
NEW JERSEY
NORTH AMERICA
PETROLOGY
ROCKS
TECTONICS
USA
VIRGINIA