![]() Horst blocks, tilted fault blocks and gentle roll-overs form the main hydrocarbon traps.ģD Seismic attributes can be of great help in delineating subsurface fault networks, their orientations and their lateral and vertical extents. Lower and Middle Indus basins of Pakistan fall in extensional to trans-tensional tectonic regime and hence are characterized by horstgraben features, tilted fault blocks and strike-slip zones with associated negative flower patterns. Keywordsĭiscontinuity attributes Seismic data Seismic interpretation Seismic attributes Introduction Many of the small faults that were not clearly visible on conventional seismic data were well highlighted using attributes’ results viewed and analyzed along time-slices as well as horizon slices. The use of mentioned attributes effectively demarcated faults’ orientations and their lateral and vertical extents. Different examples have been included, compared and explained with reference to coherence and curvature results. Coherence and curvature (most negative and most positive) cubes have been extracted using conventional Pre-stack seismic volumes after a careful selection of parameters. Coherence checks for similarity between adjacent seismic traces and can be calculated using different techniques like crosscorrelation, semblance and eigen structure measures after analyzing dips and azimuths. Apart from highlighting faults across a 3D cube, curvature attributes also give useful information about the highs and lows present in the data set that can be well correlated with the subsurface geology. Curvature attributes can be measured in different directions but mostpositive and most-negative curvature are found to be of best use in highlighting extensional regime’s geometry very effectively. This paper highlights the practical importance of curvature and coherence attributes applied on two seismic data sets (3D volumes) from Indus basin, Pakistan, both exhibiting extensional tectonics. Out of the many available discontinuity attributes, curvature and coherence have been selected because of their proven abilities to delineate faults/fractures effectively and also their suitability to the subsurface structures present in case of volumes used. There are a number of discontinuity attributes that are considered useful for identifying faults and small fractures that can’t be fully delineated using seismic amplitude data. Visit for more related articles at Oil
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