Page 167 - Hydrocarbon Exploration and Production Second Edition
P. 167

154                                                        Data Interpretation


             Relative sea level changes affect many shallow marine and coastal depositional
          environments.
             Sequence stratigraphy integrates information gleaned from seismic, cores, well
          logs and often outcrops. In many cases, it has increased the understanding of
          reservoir geometry and heterogeneity and improved the correlation of individual
          drainage units. Sequence stratigraphy has also proved a powerful tool to predict
          presence and regional distribution of reservoirs. For instance, shallow marine
          regressive surfaces may indicate the presence of turbidites in a nearby, deeper marine
          area.
             In preparation for a field wide ‘quick look’ correlation, all well logs need to be
          corrected for borehole inclination. This is done routinely with software which uses
          the measured depth (MD) below the derrick floor (‘alonghole depth’ below derrick
          floor [AHBDF] or MD) and the acquired directional surveys to calculate the true
          vertical depth subsea (TVSS). This is the vertical distance of a point below a common
          reference level, for instance chart datum (CD) or MSL. Figure 6.40 shows the
          relationship between the different depth measurements.
             To start the correlation process, we take the set of logs and select a datum plane.
          This is a marker which can be traced through all data points (three wells in the
          example of Figure 6.41). A good datum plane would be a continuous shale because
          we can assume that it represents a ‘flooding surface’ present over a wide area. Since
          shales are low-energy deposits, we may also assume that they have been deposited
          mostly horizontally, blanketing the underlying sediments thus ‘creating’ a true datum
          plane.
             Next, we align all logs at the datum plane which now becomes a straight
          horizontal line. Note that by doing so we ignore all structural movements to which
          the sequence has been exposed.











                                                         ft  =  feet
                         DFE
                                                         m   = metres
                         sea level
                                                         ss  = subsea
                                                         bdf   = below derrick floor
                                                         tv  = true vertical
                              tvss                       ah  =  along hole
                                                         TD  = total depth
                   ahbdf
                                                ahbdf    DFE = derrick floor elevation
                                   TD         TD

          Figure 6.40  Depth measurements used.
   162   163   164   165   166   167   168   169   170   171   172