COPROD2
An exercise to test two-dimensional (2D) MT inversion algorithms on the same dataset. The original data were corrected for static shifts and mildly smoothed to reduce data outliers.
Models presented in Jones (1993) derived from thirteen different inversion algortihms plus two forward trial-and-error exercises.
The COPROD2 dataset consists of magnetotelluric data from thirty-five sites on a 300-km east-west profile just north of the U.S./Canadian border in central Canada. The profile crosses the North American Central Plains (NACP) conductivity anomaly, and a smaller anomaly further to the east.
The data have been corrected for static shifts using the parametric sedimentary layer approach (see Jones, 1988). In addition, the data were mildly smoothed, to reduce outliers, using a low-order polynomial smoothing routine.
The data are stored in J-format and in EDI-format.
In each file are the ZXY and ZYX apparent resistivities and phases, plus the TZY transfer functions. The "X" direction is "North", which is geographic north in this case.
The data were used for examination at the first and second MT data interpretation workshops, MT-DIW1 and MT-DIW2.
If you use these data in a publication, please inform Alan Jones so that it can be added to the list below.
The original data, unsmoothed and uncorrected for static shifts, are also available for download to test your ideas about static shifts etc. This dataset includes all four elements of the impedance tensor for each site, and both of the vertical field responses.
NOTE: The co-ordinates in the original data files are correct. The shifted data have been moved onto an East-West line.
Download COPROD2 data
- In J-format (101 Kb zip compressed)
- In EDI-format (101 Kb zip compressed)
Download original, uncorrected, COPROD2 data
- In J-format (240 Kb zip compressed)
- In EDI-format (160 Kb zip compressed)
Published papers using COPROD2 dataset
- Jones, A.G. and Savage, J.G., 1986.
North American Central Plains conductivity anomaly goes east.
Geophysical Research Letters, 13, 685-688. - Jones, A.G., 1988.
Static shift of magnetotelluric data and its removal in a sedimentary basin environment.
Geophysics, 53, 967-978. - Jones, A.G. and Craven, J.A., 1990.
The North American Central Plains conductivity anomaly and its correlation with gravity, magnetics, seismic, and heat flow data in the Province of Saskatchewan.
Physics of the Earth and Planetary Interiors, 60, 169-194. - Morel-a-l'Huissier, P., Green, A.G., Jones, A.G., Latham, T., Majorowicz, J.A., Drury, M.J. and Thomas, M.D., 1990.
The crust beneath the intra-cratonic Williston Basin from geophysical data.
In: The Potential of Deep Seismic Reflection for Hydrocarbon Exploration, edited by B. Pinet and C. Bois, published by Les Editions Technip, 141-160. - Jones, A.G., 1993
The COPROD2 dataset: Tectonic setting, recorded MT data and comparison of models.
Journal of Geomagnetism and Geoelectricity, 45, 933-955. - Agarwal, A.K. and Weaver, J.T., 1993.
Inversion of the COPROD2 Data by a method of modelling
Journal of Geomagnetism and Geoelectricity, 45, 969-983. - deGroot-Hedlin, C. and Constable, S., 1993.
Occam's inversion and the North American Central Plains electrical anomaly
Journal of Geomagnetism and Geoelectricity, 45, 985-999. - Ellis, R.G., Farquharson, C.G. and Oldenburg, D.W., 1993.
Approximate inverse mapping inversion of the COPROD2 data
Journal of Geomagnetism and Geoelectricity, 45, 1001-1012. - Everett, M.E. and Schultz, A., 1993.
Two dimensional nonlinear magnetotelluric inversion using a genetic algorithm
Journal of Geomagnetism and Geoelectricity, 45, 1013-1026. - Rasmussen, T., 1993.
Two-dimensional Occam model of COPROD2 data - first order description of resolution and variance
Journal of Geomagnetism and Geoelectricity, 45, 1027-1037. - Schmucker, U., 1993.
2D modeling with linearized integral equations
Journal of Geomagnetism and Geoelectricity, 45, 1045-1062. - Schnegg, P.-A., 1993
An automatic scheme for 2-D magnetotelluric modelling, based on low-order polynomial fitting.
Journal of Geomagnetism and Geoelectricity, 45, 1039-1043. - Takasugi, S., Sato, T. and Honkura, Y., 1993.
Two-dimensional forward modelling for the COPROD2 MT data
Journal of Geomagnetism and Geoelectricity, 45, 957-962. - Uchida, T., 1993.
2-D inversion of COPROD2 magnetotelluric data by use of ABIC minimization method
Journal of Geomagnetism and Geoelectricity, 45, 1063-1071. - Wu, N., Booker, J.R. and Smith, J.T., 1993.
Rapid two-dimensional inversion of COPROD2 data
Journal of Geomagnetism and Geoelectricity, 45, 1073-1087. - Zhao, G, Tang, J. and Zhan, Y., 1993.
Two dimensional modelling by using COPROD2 magnetotelluric data
Journal of Geomagnetism and Geoelectricity, 45, 963-968. - Oldenburgh, D.W. and R.G. Ellis, 1993.
Efficient inversion of magnetotelluric data in two dimensions
Physics of the Earth and Planetary Interiors, 81, 177-200. - Tournerie, B., D. Gilbert and J. Virieux, 1995.
Inversion of the COPROD2 magnetotelluric data using a Diffusuve-to-Propagative Mapping (DPM).
Geophysical Research Letters, 22, 2187-2190. - Ogawa, Y. and T. Uchida, 1996.
A two-dimensional magnetotelluric inversion assuming Gaussian static shift
Geophysical Journal International, 126, 69-76. - Pous, J., Ledo, J., and Marcuello, A., 1997.
Two-dimensional forward modelling of the NACP anomaly (COPROD2R data)
Journal of Geomagnetism and Geoelectricity, 49, 739-744. - Agarwal, A.K., MacDonald, K.J., and Weaver, J.T., 1997.
COPROD2 revisited: Can the B-Polarization phase distinguish between single- and multi-body anomalies?
Journal of Geomagnetism and Geoelectricity, 49, 745-756.