I. Introduction [Narrow Azimuth OBC 3D Post Stack Time Migrated Seismic Survey on South Timbalier Block 54]:
￼We interpreted the D3 Sand within the South Timbalier 54 seismic volume to evaluate its potential for HC exploration. Various interpretation techniques were integrated to explain physical observations and anomalies. D3 Sand was deposited on the shelf in a steady to slightly dropping sea level resulting in increased in accommodation space; thus, a continuous aggradational to progradational deltaic heterogeneous sand . Seismic-wise, D3 appears as continuous layer across ST-54 with almost uniform thickness (Fig. 3 & 5), which fits with previous geological background. However, resolving its deltaic heterogeneities is beyond our seismic resolution; yet, implementing further seismic analysis could improve the detectability to resolve them.
II. Methodology [Landmark Decision Space, GeoProbe]:
We started by mimicking the seeded points on (200, 400, 600, 800 & 1000) across In-line & (50, 100, 150 & 200) along cross-line which provided us with the legacy 200x50 mesh for the top and the bottom of the D3 (Fig 1). Then, we refined the mesh down to 50x25 mesh. We altered the mesh size to minimize the effect of tracking along the low fold cross-line direction while keeping the mesh bigger within in-line where S/N is sufficient to be tracked by the software (Fig 1 & 5). Picks were made on min-phase peak assuming a min-phase data where we found coherent continuous reflection. Before tracking the mesh; we implemented user-controlled tracking process to account for the encountered irregularities within the mesh rather than using the unguided auto-tracker where we blocked tracking against polygons which were define based on anomalies driven from the attributes (Fig 1 & 2). Observed irregularities such as abrupt termination of reflectivity, mis-ties, vertical offsets & abrupt changed in seismic attributes (Amplitude, Frequency & Discontinuity) were later interpreted based on our structural & stratigraphic background of the region as faults. Results were quality controlled in 3D where we extracted the discontinuity along the fault plane (Fig 3).
Structure Analysis [Previous existing topography, Graben, generated by deep faults originated at salt diaper]:
To better illustrate our picks, let’s consider diagonal a NE-SW traverse line which orthogonally intersect most of our lateral irregularities as they commonly share a NW-SE trending. As we move from SW to NE; we observed 50 ms vertical offset within our section (Anomaly B); the offset is not unique only to our picked horizon at 1750 ms as it appears from 1100 ms all the way down to around 2400 ms or even beyond. Since data is offshore, sever near surface processing issues are excluded from our analysis and the continuity of such marginal offset in laterally and temporally indicate a major regional normal fault as those truncation does not reach the surface; instead, they gradually disperse upward. Moreover, we quality-control this interpretation ￼￼￼￼￼￼￼￼￼against a discontinuity volume where we extracted discontinuity RMS-Amplitude then transparently overlaid on the time horizon (Fig 5). Similar analogy was used to interpret anomalies B-H (Fig 5). In addition, Discontinuity volume-slicing, in 3D, showed an incoherency signature along slicing through our horizon and showed continuum discontinuities as we time-sliced our volume which supported our initial fault interpretation. Moving NE, we continued to observe these mis-tie anomalies with different magnitude and less truncation at the middle. The observed offset decreases toward the middle, then; increases sidewise. Using similar analogy to interpret those features as before, we reached a conclusion that they are mainly normal growth faults starting from zero-reflection zone beyond 2400 ms. We spot the D3 to be geometrically depressed block of sand broader by semi-parallel faults. Therefore, we interpreted the general structure to be graben. The graben is located above the center of the zero-reflectivity body, possibly the Louann Salt. Blending horizon and fault interpretation burial history, we observed that the sand could had been deposited comfortably on semi-syncline area on the top of active salt based on (Mov 1). Geological background, observed zero-reflectivity zone at the middle and the strike and dip direction of the faulting system alluded that ST54 is resides on top salt diaper/dome as the two regional major faults could be traced down to the salt; thus, originated there before the deposition of the D3 Sand . Kinematic modeling illustrated that lower strain on the sides of the graben; hence, more weight and compaction on the sides compared to the center which was the driving force behind expelling the salt upward in a semi-vertical direction in the center of the graben where the model showed higher strain; hence, more deformation at the middle of graben (Mov 1). In addition, faults strain modeling showed a higher strain on the middle indicating that those smaller faults could not be generated by salt directly; rather, they originated from other faults due to salt collapsing which is common in rapid increase of sedimentation [3,4]. Such conclusions were possible to draw considering the fact that D3 was deposited within local sea level drop during or closing of the gulf in the early stage of the graben collapsing; then, faults increase the temporal stratigraphic offset between its compartments while overall hot climate played a vital role in increasing the supply of sediments [2,3 & 4].
III. Stratigraphic Analysis [On Shelf Deltaic sand with good vertical resolution in seismic]:
Extracting the RMS-Frequency at horizons showed a dominate Frequency around 20 Hz for both yielding a vertical resolution around 30 m; assuming constant 2400 m/s at the AOI (Fig 4). Since, Frequency is inversely related to thickness; such frequency respond infer sediments diverge against the normal faults as we moved from the footwall to the hanging wall block which tie with earlier analysis.
￼IV. Hydrocarbon Potential [Yes, Bright spot in post stack seismic section with 4.12 BCF] :
￼￼￼￼￼￼Utilizing the most successfully DHI, RMS-Amplitude showed bright spots and 3 major gas pools were identify (Fig 6). Since, it is below seismic resolution to draw early conclusion about multi-producing layers within the D3; we can safely assume that the D3 is homogenous layer from reserve booking point of view only. Hence, attribute calculations are generated from the top to the bottom of the D3. Surprisingly, we did not focus our attention on the brightest area; rather, shifted our auto-polygon function cut-off value down to 4500-5200 for two main reasons (Fig 6). First, the nature of the amplitude distribution within the D3 is quite good despite contamination coming from striping effect (Fig 6). A 4500 (Highest %75-%50) is a good estimate considering that we had the same amplitude respond in A3 where we used a %35-cutoff on amplitude histogram. Moreover, D3 has been primarily in oil-production since 1979 and the tiny bright spots on the high topographic map should not correlate to leads; as they are quite small in size for associated gas and oddly fit within topographic high (Fig 4 & 6). Therefore, those tiny bright spots are secondary gas caps which were generated as result of rapid production of oil; as pressure drop during production, pushing the dissolved gas within oil upward toward topographic high while liquid is being produced. The 3 gas pools contain many leads; however, with no marginal structure change nor resolvable strata change between them, we could assume that they belong to the same gas pool but that does not necessarily mean that they are pressure-connected. On the other hand, the three pools are segregated structurally by faults; therefore, they cannot pressure communicate. In short, our pools/leads are not text-book example of 4-way closure as stratigraphic thinning beds altered the rock properties and helped defining trapping mechanism which ties with the nature of heterogeneous deltaic sand deposits in general. Using full cycle min-phase wavelet assumption, average thickness was estimated and OGIP estimate and probability were generated (Table 1).
V. Conclusion & Recommendation (Re-Processing, AVO, Inversion & Pore-Pressure Model):
Seismic interpretation and analysis provided a key role in understanding the structure style with ST-54. In addition, re- processing AVO-friendly gather should be a by-production if we decided to re-process the data as the DHI approach did not quietly represent the booked gas reserve within this field; underestimating it three time. Processing/acquisition striping artifact were observed along the cross line in amplitude attribute and interpreters should be careful as those stripes have masked the true background amplitude signature. We ought to recommend PSDM to better image the deep faulting system and the salt. Post stack seismic inversion; with enough well control, could also be beneficial to generate an accurate porosity map while Pre stack seismic inversion could also help us identify the saturated zone within the reservoir itself. Moreover, pore pressure prediction based on a seismic-velocity should be considered as it aid in optimizing the drilling program as well as the drilling mud weight design to lower the risk associated with drilling hazards.
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