Some Examples of Euler Deconvolution on Swedish Magnetic and Gravity Data

1999 ◽  
Author(s):  
L. Kero
Keyword(s):  
Gravity Data ◽  
Euler Deconvolution

scholarly journals Euler deconvolution of gravity data in Geothermal Reconnaissance; the Obama geothermal area, Japan

2006 ◽  
Vol 59 (3) ◽  
pp. 275-282 ◽  
Author(s):  
Hakim Saibi ◽  
Jun Nishijima ◽  
Essam Aboud ◽  
Sachio Ehara
Keyword(s):  
Gravity Data ◽  
Geothermal Area ◽  
Euler Deconvolution

EULDEP: a program for the Euler deconvolution of magnetic and gravity data

1998 ◽  
Vol 24 (6) ◽  
pp. 545-550 ◽  
Author(s):  
R.J. Durrheim ◽  
G.R.J. Cooper
Keyword(s):  
Gravity Data ◽  
Euler Deconvolution

scholarly journals Distribution of subsurface anomalies in the Muria Peninsula and depth analysis with euler deconvolution

2019 ◽  
Vol 3 (3) ◽  
pp. 21-30
Author(s):  
Rina Dwi Indriana
Keyword(s):  
Satellite Data ◽  
Gravity Data ◽  
The Body ◽  
Deconvolution Method ◽  
Euler Deconvolution ◽  
Central Java ◽  
Depth Analysis ◽  
East And West

Muria Peninsula is one of the regions in Central Java that is uniquely formed. The Muria Peninsula was originally separated from Java and is now connected. To complement the studies that have been done before, subsurface analysis using euler deconvolution method is carried out. Gravity data used is satellite data provided free by BGI. The results of the processing produced a residual anomaly which showed a fault that passed in the middle of the peak of Muria towards Mount Genuk. The anomaly depth of Mt. Muria is 1000 m to 2000 m, in the peak area of Muria and Genuk <1000 m, and in the east and west of the study area the anomaly depth is more than 2000 m. Euler deconvolution index 0 illustrates the body boundaries of Mt. Muria and Genuk in the form of dike and steep.

Euler deconvolution of gravity data

2003 ◽  
Author(s):  
Alan Reid ◽  
Desmond FitzGerald ◽  
Philip McInerny
Keyword(s):  
Gravity Data ◽  
Euler Deconvolution

Weighted Euler deconvolution of gravity data

Geophysics ◽  
1998 ◽  
Vol 63 (5) ◽  
pp. 1595-1603 ◽  
Author(s):  
Pierre B. Keating
Keyword(s):  
Euler Equations ◽  
Gravity Data ◽  
Error Function ◽  
Bouguer Anomaly ◽  
Depth Estimation ◽  
Euler Deconvolution ◽  
Structural Index ◽  
Eastern Canada ◽  
Adequate Sampling

Euler deconvolution is used for rapid interpretation of magnetic and gravity data. It is particularly good at delineating contacts and rapid depth estimation. The quality of the depth estimation depends mostly on the choice of the proper structural index and adequate sampling of the data. The structural index is a function of the geometry of the causative bodies. For gravity surveys, station distribution is in general irregular, and the gravity field is aliased. This results in erroneous depth estimates. By weighting the Euler equations by an error function proportional to station accuracies and the interstation distance, it is possible to reject solutions resulting from aliasing of the field and less accurate measurements. The technique is demonstrated on Bouguer anomaly data from the Charlevoix region in eastern Canada.

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