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

TY  - DATA
AB  - 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 
AU  - Moser, Mark M.
A2  - Schultz, J.
A3  - Schultz, A.
A4  - Heath, B.
A5  - Rose, Kelly
A6  - Urquhart, S.
A7  - Bowles-Martinez, E.
A8  - Vincent, P.
DB  - Geothermal Data Repository
DP  - Open EI | National Renewable Energy Laboratory
DO  - 
KW  - geothermal
KW  - enhanced geothermal system
KW  - EGS
KW  - NEWGEN
KW  - Newberry
KW  - Oregon
KW  - gravity
KW  - seismic
KW  - conceptual model
KW  - subsurface model
KW  - geologic model
KW  - structure
KW  - geophysics
KW  - faults
KW  - MT
KW  - magnetotelluric
KW  - model
KW  - conceptual
KW  - geophysical
KW  - caldera
LA  - English
DA  - 2016/03/04
PY  - 2016
PB  - National Energy Technology Laboratory
T1  - Newberry Caldera Conceptual Geophysical Model
UR  - https://gdr.openei.org/submissions/752
ER  -

Export Citation to RIS

Moser, Mark M., et al. Newberry Caldera Conceptual Geophysical Model. National Energy Technology Laboratory, 4 March, 2016, Geothermal Data Repository. https://gdr.openei.org/submissions/752.

Moser, M., Schultz, J., Schultz, A., Heath, B., Rose, K., Urquhart, S., Bowles-Martinez, E., & Vincent, P. (2016). Newberry Caldera Conceptual Geophysical Model. [Data set]. Geothermal Data Repository. National Energy Technology Laboratory. https://gdr.openei.org/submissions/752

Moser, Mark M., J. Schultz, A. Schultz, B. Heath, Kelly Rose, S. Urquhart, E. Bowles-Martinez, and P. Vincent. Newberry Caldera Conceptual Geophysical Model. National Energy Technology Laboratory, March, 4, 2016.  Distributed by Geothermal Data Repository. https://gdr.openei.org/submissions/752

@misc{GDR_Dataset_752,
title = {Newberry Caldera Conceptual Geophysical Model},
author = {Moser, Mark M. and Schultz, J. and Schultz, A. and Heath, B. and Rose, Kelly and Urquhart, S. and 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 },
url = {https://gdr.openei.org/submissions/752},
year = {2016},
howpublished = {Geothermal Data Repository, National Energy Technology Laboratory, https://gdr.openei.org/submissions/752},
note = {Accessed: 2025-05-11}
}

Details

Data from Mar 4, 2016

Last updated Nov 14, 2019

Submitted Apr 1, 2016