001     852671
005     20180929085856.0
037 _ _ |a FZJ-2018-05544
041 _ _ |a English
100 1 _ |a Adrian, Juliane
|0 P:(DE-Juel1)173971
|b 0
|u fzj
111 2 _ |a 4th International Workshop on Induced Polarization
|g IP2016
|c Aarhus
|d 2016-06-06 - 2016-06-08
|w Denmark
245 _ _ |a 2D DCR/TDIP Two-step Inversion: Detectability of ore deposits and Depth of Investigation
260 _ _ |c 2016
336 7 _ |a Conference Paper
|0 33
|2 EndNote
336 7 _ |a Other
|2 DataCite
336 7 _ |a INPROCEEDINGS
|2 BibTeX
336 7 _ |a conferenceObject
|2 DRIVER
336 7 _ |a LECTURE_SPEECH
|2 ORCID
336 7 _ |a Conference Presentation
|b conf
|m conf
|0 PUB:(DE-HGF)6
|s 1538135463_19314
|2 PUB:(DE-HGF)
520 _ _ |a The joint application of the Direct Current Resistivity (DCR) and Time-domain Induced Polarization (TDIP) methods is a helpful tool to investigate ore deposits with sulfidic content. The combined interpretation yields a resistivity and chargeability model of the subsurface which is superior to a pure resistivity model, especially when dealing with disseminated deposits.We present a newly developed smoothness constrained 2D inversion algorithm for DCR and TDIP data applying a two-step approach. It contains a Finite Element forward calculation on an unstructured triangular mesh which amongst others simplifies the incorporation of topography.The new algorithm is tested regarding the quality of the chargeability resolution with respect to the resistivity model. Furthermore, the resolution of the lower boundary of a highly chargeable model block is investigated and compared to the depth of investigation which is determined by the coverage matrix.Finally, 2D inversion results of field data acquired on a sulfidic copper ore deposit in Turkey are shown using the newly developed algorithm and a feasible interpretation is given.
700 1 _ |a Tezkan, Bülent
|0 P:(DE-HGF)0
|b 1
909 C O |o oai:juser.fz-juelich.de:852671
|p extern4vita
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 0
|6 P:(DE-Juel1)173971
980 1 _ |a EXTERN4VITA
980 _ _ |a conf
980 _ _ |a USER
980 _ _ |a I:(DE-Juel1)IAS-7-20180321


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