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India's Sedimentary Basins: Subsurface Insights        67























                                                                Source: DGH Internal
                                                              on  analogy  of  Vindhyan  Basin.  Sedimentary
                                                              thickness  of  270m  (Bhima)  and  3,000-4,500m
                                                              (Kaladgi) were envisaged.

                                                              Bhima  sub-basin  has  a  total  hydrocarbon
                                                              in-place  of  0.6  MMTOE  and  this  is  entirely
                                                              undiscovered risked in-place.
                                                              Kaladgi  sub-basin  has  a  total  hydrocarbon
                Source: DGH Internal
                                                              in-place  of  6  MMTOE  and  this  is  entirely
                                                              undiscovered risked in-place.
            Bhima-Kaladgi  are  two  Proterozoic  sub-basins
            situated  over  Dharwar  craton.  The  elements  •    Basin datasets and studies:
            of  petroleum  system  in  the  basin  are  largely
            speculative.                                      As  of  31.03.2025,  NDR  has  archived  primary
                                                              datasets  of  1,087  LKM  2D  seismic.  Multiple
            Bhima  sub-basin  is  characterized  by  Neo-     flavours of reprocessed seismic datasets are also
            Proterozoic  sedimentary  sequence  whereas  archived  whenever  the  same  are  provided  by
            Kaladgi  sub-basin  has  thick  Pale  to-Neo-     E&P Operators.
            Proterozoic   sediments.   Entire   Proterozoic
            sequences  in  Bhima-Kaladgi  Basin  has  been
            considered as single play, sub-divided into three
            assessment  units  each  on  the  basis  of  their
            respective tectonic set-up.
            Paleo-to-Meso-Proterozoic      Basuhari-Rohtas
            play  of  Vindhyan  Basin  has  been  used  in  the
            analogue  study.  Sub-basalt  imaging  to  study
            sub-trappean sediments is the focus area.

            •   Hydrocarbon prospectivity and Basin
                maturity:

            In  the  basin,  1  play  is  identified  within  Pre-
            Cambrian.  Aerial  Yield  method  was  used         Source: DGH Internal

            Basin appraisal and regime-wise active acreage:


               Location      Basin area (skm)    Appraised (skm)       Active acreage [Nos./Area (skm)]
                Kaladgi            8,820            2,616 (30%)                 No active acreage
                Bhima              5,280            5,280 (100%)                No active acreage

            The basin occupies an area of 14,101 sq km. It has been appraised to the extent of 7,896 sq km (56%)
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