% IMPORTANT: The following is UTF-8 encoded. This means that in the presence % of non-ASCII characters, it will not work with BibTeX 0.99 or older. % Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or % “biber”. @INPROCEEDINGS{Adrian:852673, author = {Adrian, Juliane and Tezkan, Bülent}, title = {{A}pplication of the {N}ewly {D}eveloped 2{D} {DCR}/{TDIP} {I}nversion {A}lgorithm: {I}nversion {S}tudiesand {A}nalysis of {F}ield {D}ata {A}cquired on a {C}opper {O}re {D}eposit}, reportid = {FZJ-2018-05546}, year = {2017}, abstract = {We present inversion studies obtained with a newly developed 2D inversion algorithm for DirectCurrent Resistivity (DCR) and Time-domain induced polarization (TDIP) data. The algorithm usesthe finite element approach on unstructured meshs which simplifies the incorporation oftopography. The model parameters resistivity and chargeability are connected by a perturbationapproach and the inversion is conducted in two steps.By inversion studies with synthetic data, it is shown that chargeability structures can be reproducedby the algorithm in presence or absence of a corresponding resistivity anomaly. A further studycompares the effects of different smoothness constraint matrices that approximate first orderderivatives of parameter transitions of neighboring mesh elements. It is shown that it is preferable touse a constraint that considers the shape and size of the elements of unstructured meshs overconstraints that weight all element boundaries equally. Furthermore, a method is presented thatapproximates a depth of investigation by deriving a threshold of sensitivity coverage from the ruleof thumb.As a case study, inversion results of field data acquired on a copper ore deposit located in Turkeyare presented. The ore deposit is elongated beneath a valley structure and has sulfide content. Dueto its disseminated form, resistivity anomalies induced by this deposit are hard to detect. However,chargeability inversion results show anomalies below 10 m depth with values of >100 mV/V. Thisclearly indicates the presence of ore with sulfide content.}, organization = {Annual Meeting of the German Geophysical Society, Potsdam (Germany)}, subtyp = {After Call}, typ = {PUB:(DE-HGF)6}, url = {https://juser.fz-juelich.de/record/852673}, }