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India's Sedimentary Basins: Subsurface Insights        41



            2.2.4 SAURASHTRA BASIN

            Saurashtra  is  a  Category  II  basin  with  sub-commercial  discovered  in-place,  potential  to  be
            commercially  produced.  The  area  geographically  overlaps  with  the  state(s)  of  Daman  and  Diu,
            Gujarat.






















                                                              Source: DGH Internal



                                                              The basin was built with Pre-Cambrian basement
                                                              overlain  by  Mesozoic  sediments  followed  by
                                                              Deccan  traps.  A  thin  cover  of  Neogene  and
                                                              Quaternary  sediments  occurs  at  the  top.  The
                                                              drainage  of  Saurashtra  shows  a  radial  pattern
                                                              from the central highland.

                                                              The source rocks maturity of Cretaceous is poor
                                                              and it remains immature in onland.
             Source: DGH Internal
                                                              Sub-basalt  imaging,  variable  basalt  thickness
                                                              and sub-optimal onland seismic data are some
            The basin is geologically contiguous with Kutch  areas of focus for exploring Cretaceous plays.
            basin and separated by the Saurashtra Arch in
            the offshore part, which trends north-northwest-  •   Hydrocarbon prospectivity and Basin
            south-southeast  direction.  The  basin  has          maturity:
            presence of prospective plays of Middle Jurassic   In the basin, 16 plays are located within Middle
            to  Early  Cretaceous  with  significant  potential   Jurassic-to-Early  Cretaceous  in  Onland  and
            of sub-basalt Mesozoic plays. There has been a    Middle  Jurassic-to-Trap-to  Middle  Miocene  in
            gas  discovery  in  Early  Cretaceous  reservoirs  at   Offshore. Petroleum system was modelled in 3D
            4,500m  depth,  below  2,500m  thick  weathered   where datasets were adequate and Aerial Yield
            basalts.  The  northerly  located  proven  Tertiary   method was used where data were limited.
            Plays of Kutch basin is extended into this basin.
                                                              Onland  sub-basin  has  a  total  hydrocarbon
            Major  part  of  Saurashtra  mainland  is  covered   in-place  of  33  MMTOE  and  this  is  entirely
            with  Deccan  Trap  basalts  with  thin  veneer  of   undiscovered  risked  in-place.  The  basin  has
            Miocene and younger sediments, exposed along      100%  of  total  in-place,  potential  to  be  explored
            Porbandar coast. The Cenozoic sediments have      and discovered.
            been  encountered  in  the  wells  drilled  in  the
            offshore Saurashtra basin. In offshore, the basin  Offshore sub-basin has a total hydrocarbon in-
            lies north of Mumbai Offshore Basin, while the  place  of  267  MMTOE.  This  includes  discovered
            onland  part  borders  with  Cambay  Basin  on  its  in-place of 70 MMTOE and undiscovered risked
            eastern  flanks.  The  deeper  offshore  Saurashtra  in-place of 197 MMTOE. The discovered in-place
            borders with the Indus fan.                       is subject to commercial development.
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