% 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{Tezkan:852796,
      author       = {Tezkan, B. and Grossbach, H. and Adrian, J. and Haroon, A.
                      and Novruzov, A.},
      title        = {{O}n the {E}exploration of {M}ud {V}olcanoes using
                      {E}lectromagnetic {T}echniques: a {C}ase {S}tudy from
                      {A}zerbaijan},
      reportid     = {FZJ-2018-05630},
      year         = {2012},
      comment      = {: [Proceedings] - , 2012. - ISBN -
                      doi:10.3997/2214-4609.20143315},
      booktitle     = {: [Proceedings] - , 2012. - ISBN -
                       doi:10.3997/2214-4609.20143315},
      abstract     = {3 mud volcanoes in Perekishkul close to Baku/ Azerbaijan
                      were chosen in order to study their conductivity structures
                      by using shallow and deep electromagnetic techniques.
                      Radiomagnetotelluric (RMT) and transient electromagnetic
                      methods were applied to study the depth range up to 150 m.
                      In order to examine depths up to 6 km, the so called long
                      offset transient electromagnetic (LOTEM) method was used.
                      RMT data were observed at 536 stations on 16 profiles
                      crossing the mud volcanoes. The RMT data were then
                      interpreted by 2D conductivity models. A 50m x 50m loop as
                      transmitter and a 20m x 20 m receiver loop were used at 72
                      stations on 6 profiles for the TEM measurements. A laterally
                      constrained inversion technique was applied on the TEM data
                      to derive a quasi-2D conductivity model.750 m dipole was
                      used as a galvanic source for the LOTEM method and a 33 A
                      current was injected. Ex and dHz/dt components were measured
                      at the receivers on a profile of the mud volcanoes. The 1D
                      joint inversion of the LOTEM Ex and TEM data clearly resolve
                      the conductivity structure up to a depth of 5 km indicating
                      a relative high resistive hydrocarbon containing layer at
                      this depth range.},
      month         = {Sep},
      date          = {2012-09-03},
      organization  = {Near Surface Geoscience 2012 – 18th
                       European Meeting of Environmental and
                       Engineering Geophysics, Paris (France),
                       3 Sep 2012 - 5 Sep 2012},
      typ          = {PUB:(DE-HGF)8 / PUB:(DE-HGF)7},
      doi          = {10.3997/2214-4609.20143315},
      url          = {https://juser.fz-juelich.de/record/852796},
}