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28     INDIA'S HYDROCARBON OUTLOOK 2024-2025



            2.1.3 MAHANADI BASIN                              Several biogenic gas fields have been discovered
                                                              with  strati-structural  entrapment  conditions.
            Mahanadi  is  a  Category  II  basin  with  sub-  Though  hydrocarbon  accumulations  often
            commercial discovered in-place, potential to be   indicate  charging  from  in-situ  shallower
            commercially produced.                            biogenic source sequences, there are instances
            The  area  geographically  overlaps  with  the    where  thermogenic  accumulations  have  been
            state(s) of Odisha.                               established.
            The  basin  is  situated  along  the  East  Coast  of   The basin hosts a thick pile of sediments, mainly
            Indian peninsula. Mahanadi basin is significantly   ranging  from  Early  Cretaceous  to  Recent.  The
            appraised with strong analogy with the easterly   basin’s  onland  part  is  mostly  covered  by  the
            located  Bengal  offshore  that  has  numerous    Mesozoic  sediments  which  is  underlying  the
            small-to-medium  discoveries.  Deepwater  has     Miocene sediments, deposited by the major river
            significant  discovered  Miocene  play  in  form   system  of  Mahanadi.  Stratigraphic  sequences
            of  discrete  and  stacked  reservoirs.  Enhanced   including  Gondwanas  are  reported  in  some
            exploration   opportunities   exists   for   the   small rift grabens.
            prospective Pliocene plays of biogenic origin.    Petroleum    system    model     results   show

            Hydrocarbon  occurrences  are  spread  over       prospective  trend  towards  northeast  part
            the  Tertiary  stratigraphic  sequences  ranging   of  offshore  adjoining  Bengal  offshore.  High
            from  the  oldest  sediments  of  Paleogene  to   resolution  seismic  acquisition  for  delineating
            the  youngest  sediments  of  Miocene-Pliocene.   deeper  plays  and  supporting  pore-pressure
                                                              study in high pressure area are the key focus.












































            Source: DGH Internal                              Source: DGH Internal
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