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  3. Audiomagnetotelluric data, Buffalo River watershed, Arkansas, 2017
  4. Audiomagnetotelluric data in the Buffalo River watershed, Arkansas, 2017; Station AMT050

Audiomagnetotelluric data in the Buffalo River watershed, Arkansas, 2017; Station AMT050

Dates

Publication Date
Start Date
2017-08-27
End Date
2017-08-27

Citation

Reitman, J., Rodriguez, B.D., and Brown, P.J., 2020, Audiomagnetotelluric data, Buffalo River watershed, Arkansas, 2017: U.S. Geological Survey data release, https://doi.org/10.5066/P9CIAXC5.

Summary

This dataset includes audio-magnetotelluric (AMT) sounding data collected in August 2017 in the Buffalo River watershed of northern Arkansas by the U.S. Geological Survey (USGS). Along with geologic mapping, the USGS used AMT data at 6 sites along a southwest-northeast profile of about 7 kilometers across the inferred northeastern margin of the Bear Creek uplift within the southern Ozark Dome to better constrain the buried, northeastern margin of the Bear Creek uplift.

Contacts

Point of Contact :
Geology, Geophysics, and Geochemistry Science Center, Brian D Rodriguez
Originator :
James Reitman, Brian D Rodriguez, Philip J Brown II
Metadata Contact :
Philip J Brown II
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase

Attached Files

Click on title to download individual files attached to this item.

USA-Arkansas-Buffalo_River-2017-AMT050.xml
Original FGDC Metadata
View 		115.45 KB application/fgdc+xml
amt050.png thumbnail 200.95 KB image/png
readme.txt 1.29 KB text/plain
AMT050 description.zip 347.48 KB application/zip
AMT050 raw data.zip 607.29 KB application/zip
USA-Arkansas-Buffalo_River-2017-AMT050.edi 57.19 KB text/plain
AMT050 calibration.zip 5.95 KB application/zip

Purpose

The purpose of this data release is to provide audio-magnetotelluric (AMT) station locations and data to the public. The primary goal of the AMT survey is to map changes in electrical resistivity with depth that are related to differences in rock type. Characterization of buried aquifers and aquitards were of primary importance to be investigated by these variations in rock types.
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