Автор |
Pratt, Thomas L. |
Автор |
Çoruh, Cahit |
Автор |
Costain, John K. |
Автор |
Glover, Lynn |
Дата выпуска |
1988 |
dc.description |
A regional seismic reflection line (I‐64) across the Virginia Piedmont has provided a stacked section suitable for an integrated interpretation of geophysical data in the region. A highly reflective upper crust, an allochthonous Blue Ridge Province, underlying thrust sheets including the Blue Ridge master decollement, and a basal decollement at a depth of about 9 km (3 s) are confirmed on the seismic data. Immediately east of the Blue Ridge Province, Appalachian structures plunge to as much as 12 km (4 s) depth. The Evington Group, Hardware terrane, and Chopawamsic metavolcanic rocks (Carolina terrane) crop out in the Piedmont Province, and numerous eastward dipping reflections originate from these rocks in the subsurface. These eastward dipping reflectors overlie a gently west dipping (10°–15°), highly reflective zone that varies in depth from 1.5 s (4.5 km) beneath the Goochland terrane to 4 s (12 km) beneath the rocks of the Evington Group. Some of the overlying eastward dipping reflections apparently root in this zone. The zone may include decollement surfaces along which the overlying rocks were transported. Relatively few reflections originate from within autochthonous Grenville basement at the western end of the profile. The Goochland granulite terrane is interpreted to be a westward thrust nappe structure that has overridden a portion of the Chopawamsic metavolcanic rocks. A broad zone of east dipping (20°–45°) reflections bounds the Goochland terrane on the east. These reflections may originate from deformation zones and continue to Moho depths. They appear to be correlative with similar events seen on other Appalachian lines. The pervasiveness of the zone of east dipping events on other seismic reflection lines and the continuity of the adjacent Piedmont gravity high suggest continuity of crustal features along the length of the Appalachians. A major conclusion of this study is that crustal thinning is responsible for the main components of the gravity field in Virginia, that is, the Appalachian gravity gradient and the Piedmont gravity high. The crust thins from about 52 km beneath the Appalachian mountains to about 35 km beneath Richmond, Virginia, and then rethickens by up to 10 km beneath the zone of east dipping reflections (mylonites?) east of Richmond. The I‐64 seismic data also contain a sequence of reflections at about 9–12 s, indicative of lower crustal layering; the base of this zone of reflections coincides almost exactly with the Mohorovicic discontinuity interpreted from earlier refraction work. The layering extends about 70 km west from Richmond, Virginia, and is interpreted as a lower crustal transition zone that is believed to persist across most of Virginia. |
Формат |
application.pdf |
Копирайт |
Copyright 1988 by the American Geophysical Union. |
Тема |
EXPLORATION GEOPHYSICS |
Тема |
Continental structures |
Тема |
GEOGRAPHIC LOCATION |
Тема |
Information Related to Geographic Region: North America |
Название |
A geophysical study of the Earth's crust in central Virginia: Implications for Appalachian crustal structure |
Тип |
article |
DOI |
10.1029/JB093iB06p06649 |
Electronic ISSN |
2156-2202 |
Print ISSN |
0148-0227 |
Журнал |
Journal of Geophysical Research: Solid Earth |
Том |
93 |
Первая страница |
6649 |
Последняя страница |
6667 |
Выпуск |
B6 |
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Wehr, F., L.GloverIII, Stratigraphy and tectonics of the the Virginia‐North Carolina Blue Ridge: Evolution of a late Proterozoic‐early Paleozoic hinge zone, Geol. Soc. Am. Bull., 96, 285–295, 1985. |
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Wernicke, B., Uniform‐sense normal simple shear of the continental lithosphere, Can. J. Earth Sci., 22, 108–125, 1985. |
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Zietz, I., J. L.Calver, S. S.Johnson, andJ. R.Kirby, Aeromagnetic map of Virginia, scale 1:500,000 ,U.S. Geol. Surv. Geophys. Inv. Map, GP‐915,1977. |