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@INPROCEEDINGS{Adrian:852667,
author = {Adrian, Juliane and Tezkan, Bülent and Candansayar, M.
Emin},
title = {2{D} {I}nversion of {DCR} and {T}ime {D}omain {IP} data: an
example from ore exploration},
school = {Universität zu Köln},
reportid = {FZJ-2018-05540},
year = {2015},
abstract = {Ore deposits often appear as disseminated sulfidic
materials. Exploring these deposits with theDirect Current
Resistivity (DCR) method alone is challenging because the
resistivity signaturescaused by disseminated material is
often hard to detect. The Time-domain Induced
Polarization(TDIP) method, on the other hand, is qualified
to detect areas with disseminated sulfidic ores dueto large
electrode polarization effects which result in large
chargeability anomalies. By employingboth methods we gain
information about both, the resistivity and the
chargeability distribution ofthe subsurface.On the poster we
present the current state of the development of a 2D
smoothness constraintinversion algorithm for DCR and TDIP
data. The implemented forward algorithm uses a FiniteElement
approach with an unstructured mesh. The model parameters
resistivity and chargeabilityare connected by either a
simple conductivity perturbation approach or a complex
conductivityapproach.As a case study, the 2D inversion
results of DCR/TDIP and RMT data obtained during a survey
ona sulfidic copper ore deposit in Turkey are presented. The
presence of an ore deposit is indicatedby areas with low
resistivity and significantly high chargeability in the
inversion models.This work is part of the BMBF/TUEBITAK
funded project ``Two-dimensional joint interpretation
ofRadiomagnetotellurics (RMT), Direct Current Resistivity
(DCR) and Induced Polarization (IP) data:an example from ore
exploration''.},
month = {Dec},
date = {2015-12-14},
organization = {2015 AGU Fall Meeting, San Francisco
(USA), 14 Dec 2015 - 18 Dec 2015},
subtyp = {After Call},
typ = {PUB:(DE-HGF)24},
url = {https://juser.fz-juelich.de/record/852667},
}