Related Datasets

Newberry Caldera Conceptual Geophysical Model

Publicly accessible License

Conceptual model for the Newberry Caldera geothermal area. Model is centered around caldera and evaluates multiple geophysical datasets to derive a conceptual subsurface model.

Includes:

Conductor layer based on transient electromagnetic data from Fitterman et al., 1988 (figure 10)
Base of conductor layer based on MT conductor values found in Waibel et al., 2014 (DOE document, figure 38)
Resistor layer based on magnetotellurics from Fitterman et al., 1988 (figure 13).
Seismic intrusives layer representing a smoothed version of 5.5 km/s seismic velocity layer defined in Beachly et al., 2012
West flank seismic body representing a fractional change in seismic velocity of 0.1, defined in Beachly et al., 2012 and Heath et al., 2015
West flank gravity body "granite" that represents a gravity anomaly identified in Waibel et al., 2014 (DOE document, figure 35)
Magma chamber defined seismically, found in Heath et al., 2015
Ring fracture fault intrusions
Various faults and geologic layers

Citation Formats

National Energy Technology Laboratory. (2016). Newberry Caldera Conceptual Geophysical Model [data set].  Retrieved from https://gdr.openei.org/submissions/752.

Export Citation to RIS

Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., and Vincent, P. Newberry Caldera Conceptual Geophysical Model. United States: N.p., 04 Mar, 2016. Web. https://gdr.openei.org/submissions/752.

Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., & Vincent, P. Newberry Caldera Conceptual Geophysical Model. United States. https://gdr.openei.org/submissions/752

Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., and Vincent, P. 2016. "Newberry Caldera Conceptual Geophysical Model". United States.  https://gdr.openei.org/submissions/752.

@div{oedi_3468, title = {Newberry Caldera Conceptual Geophysical Model}, author = {Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., and Vincent, P.}, abstractNote = {Conceptual model for the Newberry Caldera geothermal area. Model is centered around caldera and evaluates multiple geophysical datasets to derive a conceptual subsurface model. 



Includes:



Conductor layer based on transient electromagnetic data from Fitterman et al., 1988 (figure 10)

Base of conductor layer based on MT conductor values found in Waibel et al., 2014 (DOE document, figure 38)

Resistor layer based on magnetotellurics from Fitterman et al., 1988 (figure 13). 

Seismic intrusives layer representing a smoothed version of 5.5 km/s seismic velocity layer defined in Beachly et al., 2012 

West flank seismic body representing a fractional change in seismic velocity of 0.1, defined in Beachly et al., 2012 and Heath et al., 2015 

West flank gravity body "granite" that represents a gravity anomaly identified in Waibel et al., 2014 (DOE document, figure 35)

Magma chamber defined seismically, found in Heath et al., 2015 

Ring fracture fault intrusions

Various faults and geologic layers }, doi = {}, url = {https://gdr.openei.org/submissions/752}, journal = {}, number = , volume = , place = {United States}, year = {2016}, month = {03}}

Magma chamber defined seismically, found in Heath et al., 2015
Ring fracture fault intrusions
Various faults and geologic layers }, doi = {}, url = {https://gdr.openei.org/submissions/752}, journal = {}, number = , volume = , place = {United States}, year = {2016}, month = {03}}" readonly />

Details

Data from Mar 4, 2016

Last updated Nov 14, 2019

Submitted Apr 1, 2016