Three-dimensional controlled-source electromagnetic and magnetotelluric joint inversion

The growing use of the controlled-source electromagnetic method (CSEM) and magnetotellurics (MT) for exploration applications has been driving the development of data acquisition technologies, and three-dimensional (3-D) modelling and imaging techniques. However, targeting increasingly complex geolo...

Full description

Saved in:
Bibliographic Details
Published in:Geophysical journal international Vol. 178; no. 3; pp. 1305 - 1316
Main Authors: Commer, Michael, Newman, Gregory A.
Format: Journal Article
Language:English
Published: Oxford, UK Blackwell Publishing Ltd 01-09-2009
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The growing use of the controlled-source electromagnetic method (CSEM) and magnetotellurics (MT) for exploration applications has been driving the development of data acquisition technologies, and three-dimensional (3-D) modelling and imaging techniques. However, targeting increasingly complex geological environments also further enhances the problems inherent in large-scale inversion, such as non-uniqueness and resolution issues. In this paper, we report on two techniques to mitigate these problems. We use 3-D joint CSEM and MT inversion to improve the model resolution. To avoid the suppression of the resolution capacities of one data type, and thus to balance the use of inherent, and ideally complementary information content, different data reweighting schemes are proposed. Further, a hybrid model parametrization approach is presented, where traditional cell-based model parameters are used simultaneously within a parametric inversion. The idea is to limit the non-uniqueness problem, typical for 3-D imaging problems, in order to allow for a more focusing inversion. The methods are demonstrated using synthetic data generated from models with a strong practical relevance.
Bibliography:ark:/67375/HXZ-7CSL5T5W-H
istex:EB9C2433A4062641CB74AD269E1154089115A343
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
Earth Sciences Division
LBNL-1757E
DE-AC02-05CH11231
ISSN:0956-540X
1365-246X
DOI:10.1111/j.1365-246X.2009.04216.x