3D resistivity gridding of large AEM datasets: A step toward enhanced geological interpretation

被引:22
|
作者
Pryet, Alexandre [1 ]
Ramm, James [2 ]
Chiles, Jean-Paul [3 ]
Auken, Esben [2 ]
Deffontaines, Benoit [4 ]
Violette, Sophie [1 ]
机构
[1] Univ Paris 06, CNRS, UMR Sisyphe, F-75252 Paris 05, France
[2] Univ Aarhus, HydroGeophys Grp, Dept Earth Sci, DK-8000 Aarhus C, Denmark
[3] MINES ParisTech, Ctr Geosci & Geoengn, Fontainebleau, France
[4] UPE, GTMC Lab, Marne La Vallee, France
关键词
Airborne electromagnetics; 3D resistivity model; 3D grid; Kriging; Interpolation; AIRBORNE ELECTROMAGNETIC DATA; CONSTRAINED INVERSION; TEM DATA; AUSTRALIA;
D O I
10.1016/j.jappgeo.2011.07.006
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We develop a technique allowing 3D gridding of large sets of 1D resistivity models obtained after inversion of extensive airborne EM surveys. The method is based on the assumption of a layered-earth model. 2D kriging is used for interpolation of geophysical model parameters and their corresponding uncertainties. The 3D grid is created from the interpolated data, its structure accurately follows the geophysical model, providing a lightweight file for a good rendering. Propagation of errors is tracked through the quantification of uncertainties from both inversion and interpolation procedures. The 3D grid is exported to a portable standard, which allows flexible visualization and volumetric computations, and improves interpretation. The method is validated and illustrated by a case-study on Santa Cruz Island, in the Galapagos Archipelago. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:277 / 283
页数:7
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