Time Domain Survey of the Los Alamos Region, New Mexico

A time domain electromagnetic sounding survey of the region surrounding the city of Los Alamos, New Mexico was carried out. The results show that a linear trough, trending northeast--southwest runs beneath the city. The southern boundary is somewhat to the south of the city, the northern boundary was not established. The geoelectric section consists of three layers and the total thickness of the section is in excess of 3 000 m. The resistivities of the second layer are as low as 2.5 ..cap omega.. m. If the salinities are in the region of 7 000 ppm, the resistivities could indicate that water with a temperature of 150/sup 0/C may be found at a depth of 3 000 m. Library ID#=oitGHC_0220-01.

Data and Resources

Metadata Source

Additional Info

Field Value
Citation Date 1979-06-01T00:00:00

Harvest Information

Original ID 3F032C6EA6324210919AC7814DAAFD03
Index Date 2016-03-17T20:53:10
Original Format ISO-USGIN
Original Version 1.2

Author

Name Williston, McNeiI and Associates
Organization Los Alamos Scientific Laboratory of the University of California, Los Alamos, NM (USA)
Email geoheat@oit.edu

Geographic Extent

North Bound 37
South Bound 31.33
East Bound -103
West Bound -109.05