License P1359
Transcription
License P1359
License P1359 23rd Licence Round Promote Two Year Report Blocks 49/2c, 3b, 4d Wintershall Noordzee BV (100%) December 2007 Synopsis The current Promote Two Years Report has been written in support of the relinquishment of the licence following a detailed investigation of its Carboniferous exploration potential. Because no viable economic prospect could be defined during the first phase of the Initial Term the operator has chosen not to commit to drill a well during the second phase of the Initial Term and to relinquish the licence. After detailed investigation two of the three prospects, Ketex South and Alpha, which were recognised at the time of the licence application, were discarded as viable prospects. The volumes of the third prospect, Marjan, are too low to form an economic viable drilling candidate. Exploration Activities Wintershall was awarded Licence P1359 in the 23rd Licensing Round. After the application was granted in January 2006, the following exploration activities have been undertaken: For seismic interpretation the PGS SNS MegaMerge 3D survey was used and key horizons have been interpreted, such as the base Zechstein, the base Permian Unconformity (BPU) and the top Early Westphalian B. A regional velocity study was carried out using data from ca. 150 wells, which resulted in an improved velocity model: Interval Function Constants V0 Grid values North Sea Group V=V0+k*z k = 0.37 V0 = 1646 – 1900 Chalk V=V0+k*z k = 1.30 V0 = 1549 – 2475 Triassic V=V0+k*z k = 0.39 V0 = 2586 – 3176 Zechstein Wedge Model d = Vst + c c = 25 Vs = 4400 Rotliegend Constant velocity Vint = 4300m/sec Carboniferous Constant velocity Vint = 4300m/sec Table 1 Velocity model A regional Carboniferous reservoir study was carried out, which resulted in a detailed zonation (Fig. 2). Well data were used to create zonal isopachs. These were subsequently used to create a detailed subcrop map at the BPU level (Fig 3). This facilitated the identification of sections with good reservoir quality within BPU closure and possible stratigraphic trapping configurations. Promote Two Year Report, Blocks 49/2c, 3b, 4d Prospectivity Analysis The BPU horizon is complicated to interpret in the northern Quad 49 blocks in areas with poor seismic quality. During the present study the horizon has been interpreted in detail and was converted to depth with the improved velocity model. This affected the size and outlines of the prospects as presented in the application report (Fig. 4). In general, the source rock presence, maturity and charge are no major concern in the license area, since every valid structural test in the Silverpit Basin showed to be gasbearing. The main risks lie in trap effectiveness and reservoir presence. The presence of the Lower Leman sandstone, as demonstrated by well 49/8-2, causes the stratigraphic traps to fail as is the case for the Ketex and Alpha prospects. Additionally, 49/8-2 showed tight gas in the Westphalian C. Although decreased in size, the remaining prospectivity of the licence lies in the Marjan prospect. P1359 Figure 1 Location map. Promote Two Year Report, Blocks 49/2c, 3b, 4d Figure 2 Carboniferous stratigraphy. Promote Two Year Report, Blocks 49/2c, 3b, 4d 2°24’00” 2°36’00” 54°00’00” 2°12’00” Ketex South 53°50’00” Marjan Alpha Subcrop map at Base Permian Unconformity (BPU) (for legend see Fig. 2). 54°00’00” Figure 3 Ketex South 53°50’00” Marjan Alpha 2°12’00” 2°24’00” Figure 4 2°36’00” Base Permian Unconformity depth map Promote Two Year Report, Blocks 49/2c, 3b, 4d Alpha (Fig. 5) The Alpha prospect relies on a Westphalian C pinch-out trap with Silverpit top seal and Westphalian B bottom seal to the east and south. The triangular structure spills at 3650 m along the northwestern edge. The Carboniferous zonation study showed that the pinch-out of the EWC sands could be drawn slightly further south than originally mapped. However, the trap will fail with the presence of the Lower Leman sandstone. Given the close position to well 49/8-2 and 49/9-6z this is very likely. The stratigraphic trapping mechanism for this prospect is therefore unlikely and thus reducing the chance of success for the prospect. BPU depth map Figure 5 Prospect details Alpha Marjan (Fig. 6) A base Silverpit trap with a closing contour of 3860 m forms the Marjan prospect. The detailed interpretation of the BPU horizon and an adjusted velocity model resulted in a slightly different prospect outline and a lower vertical closure when compared to the application report, with 88% of the gross rock volume between 3860 and 3800 meters. Previous problems to close the structure in the southeast corner, related to the interpretation of a narrow ridge, are still a concern in the new model. For well 49/2-4z a GWC of 3860 m is given in the end-of-well report, but reevaluation of the data cannot support this interpretation. Most pressure points of 49/24z plot along a water line, with a possible gas point at 3775 m. The gas line through this point intersects the water line at 3860 m. However, the pressure point on the gas line shows tight gas and the pressure test was abandoned. The log data of well 49/2-3 Promote Two Year Report, Blocks 49/2c, 3b, 4d also indicate an isolated gas pocket in a sandstone layer at 3855 m. However, the pressure points of 49/2-3 all plot along a waterline, and the water saturation values show that the well is water bearing up to 3820 m. A sample taken from 3835 m contained only formation water and drilling fluids. The issue was raised previously that the eastern and western parts of the Marjan prospect may or may not be connected along a narrow zone separated by a NW-SE trending fault. The model shows only limited offset along the BPU depth map Figure 6 Prospect details Marjan fault and the throw is insufficient for fault sealing to be likely. This strengthens the case for an overall WUT level of 3820 m. The two wells drilled in the structure both show poor quality Westphalian C reservoir. Both wells mainly intersect the lower shaley part of the LWC. The new model confirms that along the edges of the prospect the LWC thickens, which brings the more sandy upper part of the LWC into closure, albeit no significant part will be above 3820 m. Reserves Summary A volumetric assessment of the Marjan prospect is presented below. No volumes were calculated for the Alpha and Ketx South prospects, since these are no longer considered to be valid prospects. Marjan P10 P50 P90 GIIP (Bcm) Reserves (Bcm) POS = 25% 2.6 1.6 1.5 0.9 0.9 0.5 Promote Two Year Report, Blocks 49/2c, 3b, 4d Promote Two Year Report, Blocks 49/2c, 3b, 4d