Southwest extension of dextral transpression along the Burnsville fault into the Clyde 7.5-minute quadrangle, western North Carolina, USA
The Neoacadian Burnsville fault is a dextral transpressional structure exposed in western North Carolina. Bedrock geologic mapping in the Clyde 7.5-minute quadrangle documents the fault an additional ∼40 km southwest than previously mapped. Here it overprints the contact between the Ashe Metamorphic...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Taylor & Francis Group
2020-12-01
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Series: | Journal of Maps |
Subjects: | |
Online Access: | http://dx.doi.org/10.1080/17445647.2020.1737255 |