Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada
Data are presented for 17 stations. The frequency used was from 7.5 to 18,600 Hz. (WHK)
Two magnetotelluric soundings (MTS) were made in the Darrough Hot Springs area, one at the hot springs (38/sup 0/ 49' 29'' latitude, 117/sup 0/ 10' 55'' longitude) and the other four miles east (38/sup 0/ 49' 20'' latitude, 117/sup 0/ 06' 30'' longitude) of the hot springs. The Cagniard resistivities are tabulated along with the audio-magnetotelluric data for the hot springs and the one-dimensional model apparent resistivities derived from the data. The MTS data (.01 to .3 Hz) is strongly anisotropic with the north-south (rho x) resistivities being approximately a factor of ten greater than the east-west (rho y) resistivities for the lower frequencies.
O'Donnell, J.E.. Magnetotelluric soundings in the Darrough Hot Springs area, Nevada. United States: N. p., 1976.
Web. doi:10.2172/7138535.
O'Donnell, J.E.. Magnetotelluric soundings in the Darrough Hot Springs area, Nevada. United States. doi:10.2172/7138535.
O'Donnell, J.E.. Thu .
"Magnetotelluric soundings in the Darrough Hot Springs area, Nevada". United States.
doi:10.2172/7138535. https://www.osti.gov/servlets/purl/7138535.
@article{osti_7138535,
title = {Magnetotelluric soundings in the Darrough Hot Springs area, Nevada},
author = {O'Donnell, J.E.},
abstractNote = {Two magnetotelluric soundings (MTS) were made in the Darrough Hot Springs area, one at the hot springs (38/sup 0/ 49' 29'' latitude, 117/sup 0/ 10' 55'' longitude) and the other four miles east (38/sup 0/ 49' 20'' latitude, 117/sup 0/ 06' 30'' longitude) of the hot springs. The Cagniard resistivities are tabulated along with the audio-magnetotelluric data for the hot springs and the one-dimensional model apparent resistivities derived from the data. The MTS data (.01 to .3 Hz) is strongly anisotropic with the north-south (rho x) resistivities being approximately a factor of ten greater than the east-west (rho y) resistivities for the lower frequencies.},
doi = {10.2172/7138535},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Thu Jan 01 00:00:00 EST 1976},
month = {Thu Jan 01 00:00:00 EST 1976}
}