The extended Euler deconvolution algorithm is shown to be a generalization and unification of 2-D Euler deconvolution and Werner deconvolution. After recasting the extended Euler algorithm in a way that suggests a natural generalization to three dimensions, we show that the 3-D extension can be realized using generalized Hilbert transforms. The resulting algorithm is both a generalization of ex...

following a magnetic survey in saghande yazd region, the existance of a relatively important dike shape anomaly was detected. in the present study, this anomaly has been interpreted by the werner deconvolution method and parker standard curves. the location and depth of the uper surface of magnetic dike has been calculated by the werner method using a series of profiles perpendicular to the str...

depth estimation of the top of the bedrock in the sedimentary basins is the main goal in geomagnetic explorations. the depth estimation of this kind of anomalies can be done using different methods, in the cases where the bedrock is magnetized. in this article, we use the standard euler deconvolution method and its results to interpret the magnetic data from the reshm region in semnan province ...

Abstract Qualitative interpretation is one of the most important missions in geophysical methods, particularly determination shape and depth disturbing bodies. The characteristics gravity field make it difficult to unequivocally determine both these parameters; therefore, problem solved by reducing body means simple solid figures on this basis an attempt estimate their depth. This paper present...

In this study, the analysis of ground gravity data (from Libyan Petroleum Institute) and aeromagnetic African Magnetic Mapping Project) are used to delineate structure elements basement depth within Jifara plain, northwest Libya. A high-pass filter a reduction-to-the-pole (RTP) transformation applied respectively. The Total horizontal gradient Centre for Exploration Targeting (CET) grid dataset...

DOI:10.17014/ijog.9.2.209-217 Determination of the straight down range geologic formation between geographic latitude 8.30 0 N to 9 and longitude 3.30 E 4.30 Igbeti schist belt became a thing interest due on-going exploration in region. Aeromagnetic field intensity anomaly data bound were then acquired, separated off regional corresponding residual map obtained was later used applying Werner de...

Diffusion tensor imaging (DTI) MRI is a noninvasive imaging method of the cerebral tissues whose fibers directions are not evaluated correctly in the regions of the crossing fibers. For the same reason the high angular resolution diffusion images (HARDI) are used for estimation of the fiber direction in each voxel. One of the main methods to specify the direction of fibers is usage of the spher...