Flowage and recrystallization in paleozoic quartzites

Eos, Transactions, American Geophysical Union
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Abstract

The lower limit of visible traces of penetrative movement in quartz‐rich rocks can be defined by studies of orientations and mutual relations of grains. Intensity of deformation in the central Appalachians decreases gradually from the crystalline Piedmont toward the north, northwest, and west perpendicular to the regional trend. The author has attempted to determine the limits of visible deformation geographically and stratigraphically.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Flowage and recrystallization in paleozoic quartzites
Series title Eos, Transactions, American Geophysical Union
DOI 10.1029/TR024i001p00271-1
Volume 24
Issue 1
Year Published 1943
Publisher American Geophysical Union
Description 1 p.
First page 271
Last page 271
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