Depth
Maps
Calibration Using Fluid Contact Evidences: A Case History
By
M. Serazzi1, F. Marchini1
(1) ENI SpA - Agip Division, S. Donato Milanese, Italy
Conformity to trap geometry is usually required for validating seismic amplitude anomalies and flat spot reflections as Direct Hydrocarbon Indicators.
This case history refers to an offshore field, where the interpretation of reprocessed seismic, supported by seismic modelling and sedimentology revision, allowed to recognise DHIs with high confidence.
Inconsistencies with structural map have therefore been interpreted as zones
of poor map precision, and utilised for
depth
map calibration, providing a tool
for improving geophysical
maps
precision.
The field is characterised by two culminations separated by a saddle. The reservoir is very uniform in terms of thickness and petrophysical properties, and extends continuously all over the area. The pay area shows clear amplitude anomaly.
Two types of calibration have been implemented:
1. saddle area. We modelled the relation between amplitudes and gross pay,
due to interference between top reservoir and OWC reflections. An
amplitude-based gross pay map has been produced, that, added to the OWC
depth
,
provides the reservoir top in the OWC area. The maximum correction was -80 ft.
2. flank area. A clear flat-spot is visible, which towards the Northern
structure
significantly departs from
depth
contours. The map has been forced to
OWC
depth
along the intersection between reservoir top and flat spot
reflections, significantly modifying the mapped dip and azimuth. The maximum
correction along the flat-spot is -150 ft.
A well drilled close to the flank hit the top reservoir with only 9 ft error, compared with 35 ft of the map calibrated with wells only.
