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@ARTICLE{Inan:201138,
      author       = {Inan, S. and Ugur, F. Alp and Inan, T. and Yalçin, M. N.
                      and Mann, U.},
      title        = {{RELATIONSHIP} {BETWEEN} {ORGANIC} {MATTER}, {SULPHUR}
                      {AND} {PHOSPHATE} {CONTENTS} {IN} {UPPER} {CRETACEOUS}
                      {MARINE} {CARBONATES} ({KARABOGAZ} {FORMATION}, {SE}
                      {TURKEY}): {IMPLICATIONS} {FOR} {EARLY} {OIL} {GENERATION}},
      journal      = {Journal of petroleum geology},
      volume       = {33},
      number       = {4},
      issn         = {0141-6421},
      address      = {Oxford [u.a.]},
      publisher    = {Wiley-Blackwell},
      reportid     = {FZJ-2015-03443},
      pages        = {319 - 337},
      year         = {2010},
      abstract     = {In this paper, we discuss the relationship between the
                      organic matter, sulphur and phosphate contents of Upper
                      Cretaceous marine carbonates (Karabogaz Formation) in the
                      Adiyaman Petroleum Province of SE Turkey. The results of
                      organic geochemical analyses of core samples obtained from
                      the Karabogaz Formation suggest that phosphate deposition
                      occurred in settings where the water column was oxic to
                      sub-oxic. However, the preservation of organic matter was
                      favoured in anoxic environments. Moreover, the presence of
                      sulphur (especially sulphur incorporated into kerogen) in
                      organic matter-rich layers led to early oil generation. The
                      results of stepwise py-gc analyses are consistent with a
                      model in which, with increasing maturity, S-S and C-S bonds
                      are the first to be eliminated from the macromolecular
                      kerogen structure. Study of the maturity evolution of S-rich
                      kerogen by laboratory pyrolysis implies that marginally
                      mature and/or mature kerogen in the Karabogaz Formation,
                      which may be classified as classic “Type II” kerogen,
                      was most probably Type II/S at lower maturity stages. This
                      enabled oil generation to occur at relatively shallow burial
                      depths and relatively early stages of maturation. It is
                      reasonable to conclude that Type II/S kerogen, overlooked in
                      previous studies, was abundant in TOC-rich intervals in the
                      Karabogaz Formation. Early generation (and expulsion) from
                      Type II/S kerogen may have sourced the sulphur-rich oils in
                      the Adiyaman area oilfields.},
      cin          = {IBG-3},
      ddc          = {620},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {246 - Modelling and Monitoring Terrestrial Systems: Methods
                      and Technologies (POF2-246) / 255 - Terrestrial Systems:
                      From Observation to Prediction (POF3-255)},
      pid          = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000282183600003},
      doi          = {10.1111/j.1747-5457.2010.00482.x},
      url          = {https://juser.fz-juelich.de/record/201138},
}