Evidence for Cenozoic topographic rejuvenation associated with the Laurel Creek Lineament in the Spruce Pine 7.5-minute quadrangle, western North Carolina, USA-Reference-Cited by-同舟云学术

Evidence for Cenozoic topographic rejuvenation associated with the Laurel Creek Lineament in the Spruce Pine 7.5-minute quadrangle, western North Carolina, USA

Published:2023-11-18 Issue:1 Volume:19 Page:
ISSN:1744-5647
Container-title:Journal of Maps
language:en
Short-container-title:Journal of Maps

Author:

Langille Jackie M.¹,Palmer Megan¹,Green Chloe¹

Affiliation:

1. Department of Environmental Science, University of North Carolina at Asheville, Asheville, NC, USA

Funder

U.S. Geological Survey

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geography, Planning and Development

Link

https://www.tandfonline.com/doi/pdf/10.1080/17445647.2023.2280594

Reference27 articles.

1. The Ashe Metamorphic Suite, Northwest North Carolina; metamorphism and observations on geologic history

2. Geomorphic evidence for persistent, cumulative deformation of the Virginia Piedmont in the vicinity of the 23 August 2011 Mineral earthquake

3. Relationship between observed upper mantle structures and recent tectonic activity across the Southeastern United States

4. Brobst D. A. (1962). Geology of Spruce Pine district Avery Mitchell and Yancey counties North Carolina . U.S. Geological Survey Bulletin B-1122-A scale 1:24.000.

5. Arrested development: Erosional equilibrium in the southern Sierra Nevada, California, maintained by feedbacks between channel incision and hillslope sediment production

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