Model-independent depth estimation with the SPI ™ method

1999 SEG Annual Meeting

Volumn , Issue , 1999, Pages

  Thurston, Jeffrey B ^a   Smith, Richard S ^a   Guillon, Jean Claude ^b  

^a Geoterrex Dighem   (Canada)

^b NONE

Author keywords

[No Author keywords available]

Indexed keywords

AEROMAGNETIC DATA; CRYSTALLINE BASEMENT; DEPTH ESTIMATION; HORIZONTAL CYLINDERS; LEAST SQUARES TECHNIQUES; MODEL ASSUMPTIONS; MODEL INDEPENDENT; STRUCTURAL INTERPRETATION;

EID: 85061459085     PISSN: None     EISSN: None     Source Type: Conference Proceeding    
DOI: None     Document Type: Conference Paper

References (7)

1. Cant, D. J., 1988, Regional structure and development of the Peace River Arch: A paleozoic failed-rift system?: Bull. Can. Petr. Geol., 36, 284-295.
2. Gay, S. P., 1963, Standard curves for the interpretation of magnetic anomalies over long tabular bodies: Geophysics, 28, 161-200
3. Grant, F. S., and West, G. F., 1965, Interpretation theory in applied geophysics: New York, McGraw-Hill Book. Inc.
4. Nabighian, M. N., 1972, The analytic signal of two-dimensional magnetic bodies widi polygonal cross-section; Its properties and use for automated interpretation: Geophysics, 37, 507-517.
5. Ross, G. M., Parrish, R.., Villeneuve, M. E., and Bowring, S. A, 1991, Geophysics and geochronology of the crystalline basement of the Alberta Basin, western Canada: Can. J. Earth Sci., 28, 512-522.
6. ™ - The improved Source Parameter Imaging method: Geophysical Prospecting, 46, 141-151.
7. Thurston, J. B., and Smith, R. S., 1997, Automatic conversion of magnetic data to depth, dip, and susceptibility contrast using the SPI (TM) method: Geophysics, 62, 807-813.