Quantifying Depth-Dependent Seismic Anisotropy in the Critical Zone Enhanced by Weathering of a Piedmont Schist Data

Authors:
Benjamin Eppinger
Owners: Benjamin Eppinger
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Created: May 27, 2021 at 7:37 p.m.
Last updated: May 28, 2021 at 3:46 a.m.
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Abstract

Article Title: Quantifying Depth-Dependent Seismic Anisotropy in the Critical Zone Enhanced by Weathering of a Piedmont Schist

Authors: B.J. Eppinger, J.L. Hayes, B.J. Carr, S. Moon, C. Cosans, W.S. Holbrook, C.J. Harman, and Z.T. Plante

Corresponding author: Jorden L. Hayes (hayesjo@dickinson.edu)

These files contain all near-surface geophysical data used in our paper titled "Quantifying Depth-Dependent Seismic Anisotropy in the Critical Zone Enhanced by Weathering of a Piedmont Schist". These data include geophone readings for 4 seismic refraction profiles and 14 circular seismic refraction surveys. The data is grouped by the location at which it was collected and the site names correspond to those used in the aforementioned paper.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Oregon Ridge Park
Longitude
-76.6824°
Latitude
39.4818°
Marker
Leaflet Map data © OpenStreetMap contributors

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How to Cite

Eppinger, B. (2021). Quantifying Depth-Dependent Seismic Anisotropy in the Critical Zone Enhanced by Weathering of a Piedmont Schist Data, HydroShare, http://www.hydroshare.org/resource/541124a1dbca409fb6a29b8f35fb3c01

This resource is shared under the Creative Commons Attribution CC BY.

 http://creativecommons.org/licenses/by/4.0/
CC-BY

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