weights of evidence.zip
This was used as a layer of evidence for weights of evidence analysis to develop a probabilistic geothermal play fairway analysis model of the Tularosa Basin, New Mexico for Phase 2 PFA. The data have been re-interpolated for Phase 2 including the new data acquired in the Tularosa Basin area, making this dataset different than the the temperature gradient data used in Phase 1. The results were classified using 1/3 standard deviation to create 12 classes where high values indicate high temperature gradients and low values indicate low temperature gradients.
|Last updated||July 11, 2017|
|Created||July 11, 2017|
|License||Creative Commons Attribution 4.0|
|created||over 2 years ago|
|resource group id||d8ed6873-725f-4d11-af10-084565d87fb9|