Virginia City Cole Surface/Borehole Microseismic Monitor Program

2015 ◽  
Author(s):  
Joe Teff ◽  
Brendan Elliott ◽  
Jarret Borell ◽  
David Langton ◽  
Richard Hand ◽  
...  
Keyword(s):  
Virginia City ◽  
Surface Borehole ◽  
Monitor Program

Virginia City Cole Surface/Bore-Hole Microseismic Monitor Program

2015 ◽  
Author(s):  
Joe Teff ◽  
David Langton ◽  
Tanner Womack ◽  
Bill Greenlees ◽  
Jarret Borell ◽  
...  
Keyword(s):  
Virginia City ◽  
Monitor Program

Virginia City

2012 ◽  
Author(s):  
Ronald M. James
Keyword(s):  
Virginia City

Mark Twain in Virginia City

1964 ◽  
Vol 51 (3) ◽  
pp. 511
Author(s):  
Richard G. Lillard ◽  
Paul Fatout
Keyword(s):  
Mark Twain ◽  
Virginia City

scholarly journals The Forward Modeling for Surface-borehole Observation Responses of Polarized Target

2021 ◽  
Vol 2078 (1) ◽  
pp. 012035
Author(s):  
Qingxin Meng ◽  
Zhigang Wang ◽  
Yao Lu ◽  
Guoyuan Hang
Keyword(s):  
Time Spectrum ◽  
Induced Polarization ◽  
Polarization Method ◽  
Geoelectric Model ◽  
Polarized Target ◽  
Similar Work ◽  
Resource Exploration ◽  
Different Depths ◽  
Surface Borehole ◽  
Main Change

Abstract Surface-hole induced polarization method is a typical deep resource exploration technology, which plays an important role in the mineral survey. The traditional surface-hole induced polarization method is mainly to observe a single polarized secondary field. At present, the time spectrum observation of polarization fields is becoming more and more popular, which greatly enriches the interpretation technology of induced polarization data. In this work, the time spectrum induced polarization method is expounded, the decay polarization fields were numerical calculated and analyzed for the typical 2-dimensional geoelectric model. The results show that for a single polarized target, the time spectrum obtained from different azimuth observation responses are basically the same, which can effectively reflect the time-varying characteristics of the polarized fields. The observation responses of polarized target at different depths can still reflect the time spectrum of decay fields. The main change of the observed response of the polarized target closer to the borehole is the response amplitude. The conclusions and simulations of this study can provide working mode for relevant research and reference for similar work.

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