% 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”.

@ARTICLE{Adrian:909309,
      author       = {Adrian, Juliane and Tezkan, Bülent and Candansayar, M.
                      Emin},
      title        = {{E}xploration of a {C}opper {O}re {D}eposit in
                      {E}lbistan/{T}urkey {U}sing 2{D} {I}nversion of the
                      {T}ime-{D}omain {I}nduced {P}olarization {D}ata by {U}sing
                      {U}nstructured {M}esh},
      journal      = {Pure and applied geophysics},
      volume       = {179},
      number       = {6-7},
      issn         = {0033-4553},
      address      = {Basel},
      publisher    = {Birkhäuser},
      reportid     = {FZJ-2022-03118},
      pages        = {2255 - 2272},
      year         = {2022},
      abstract     = {We present the results of a direct current (DC)resistivity
                      and time-domain induced polarization (TDIP) surveyexploring
                      a copper ore deposit in Elbistan/Turkey. The ore depositis
                      elongated below a valley and is of disseminated form with
                      sulfidecontent. DC and IP data were acquired using the
                      pole-dipole arrayon eight parallel profiles crossing the
                      valley perpendicularly. Thelength of each profile was 300 m
                      with an inter-profile distance ofabout 50 m. The data were
                      interpreted by a newly developed 2DDC/TDIP inversion
                      algorithm. The finite element algorithm uses alocal
                      smoothness constrained regularization on unstructuredmeshes.
                      The finite element forward solution, as well as the
                      inverseproblem, is solved by an iterative preconditioned
                      conjugate solver.The depth of investigation (DOI) was
                      determined from cumulativesensitivities of the 2D inversion
                      algorithm results. Because of thedissemination of the ore,
                      the 2D inversion of the DC data wasambiguous: However, due
                      to the sulfide content, a strong chargeabilityanomaly
                      associated with the ore body was detected. Weshow that
                      chargeability anomalies can generally be detected in
                      theabsence or presence of corresponding resistivity
                      anomalies. Thishighly chargeable structure was confined in
                      lateral direction.Although the lower boundary of the
                      structure could not be resolvedby the applied field set-up,
                      a rough estimation of it could be derivedat a depth of 90 m
                      using synthetic modeling analyses. The 2Dchargeability
                      models are consistent with existing boreholeinformation.},
      cin          = {IAS-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IAS-7-20180321},
      pnm          = {5111 - Domain-Specific Simulation $\&$ Data Life Cycle Labs
                      (SDLs) and Research Groups (POF4-511)},
      pid          = {G:(DE-HGF)POF4-5111},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000817000100001},
      doi          = {10.1007/s00024-022-03071-3},
      url          = {https://juser.fz-juelich.de/record/909309},
}