评估Wd-8租赁作业区块的下游和中下游地层

Mark Emmanuel Bishop, W. Lalla, X. Moonan
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摘要

WD-8区块位于森林储备油田内。森林保护区以ne - wsw走向而闻名,东南边缘的森林保护区背斜落入NW-SE走向的洛斯巴霍斯断层。从区域上看,森林保护区背斜的南部是向西南倾斜的Siparia向斜,森林保护区背斜的北部是Morne L ' Enfer向斜。WD-8位于森林保护区背斜的北侧,背斜的轴线位于地块的南部。在2018年之前,TETL最后一次在WD-8区块内钻探是在2014年。2018年之前,WD-8区块内的钻井主要集中在区块南部。2018年,TETL在WD-8区块北部钻了5口井。这些井的结果促使对WD-8区块北部进行评估,以确定Lower Cruse和Navet油藏的结构和范围。2018年在该区块内进行的现场宽测显示,Cruse层的砂体趋势为WSW-ENE方向,WD-8北部的砂体非常窄,最大宽度在100英尺至150英尺之间。此外,研究表明,使用较小的井距,井会遇到相邻井中未见的不同产砂体。南段与北段下部井砂体特征也存在差异。WD-8块体南部下河段倾向于形成较厚的斜坡河道堆积砂体,而北部则倾向于形成较薄的斜坡河道堆积砂体。构造上还发现南井与北井之间存在一条ENE-WSW断裂。在WD-8北部,在晚中新世Lower Cruse组下方发现始新统Navet组地层异常。该区块北部的两口井发现了Navet地层的抗阻性,只有一口井对该储层进行了测试。这就提出了一个新的未开发目标储层。通过对Navet组的测图可知,该储层走向为WSW-ENE方向。通过更新WD-8区块的地质模型,确定了6口开发井,以进一步开发WD-8区块Lower Cruse和Navet地层的剩余储量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluating the Lower Cruse and Navet Formations Within the Wd-8 Lease Operatorship Block
Lease Operatorship block WD-8, lies within the Forest Reserve oilfield. Forest Reserve is known for having the ENE-WSW trending, south easterly verging Forest Reserve anticline which plunges into NW-SE trending Los Bajos Fault. Regionally to the south of the Forest Reserve anticline lies the south westerly plunging Siparia syncline and to the north of the Forest Reserve anticline is the Morne L′ Enfer syncline. WD-8 is situated on the northern flank of the Forest Reserve anticline with the axis of the anticline occurring within the southern part of the block. Prior to 2018, TETL last drilled within the WD-8 block in the year 2014. Drilling within the WD-8 block pre-2018 was mainly in the southern portion of the block. The year 2018 saw TETL drill five wells in the northern part of the WD-8 block. The results from these wells prompted an evaluation within the Northern portion of the WD-8 block to determine the structure and extent of the Lower Cruse and Navet reservoirs. Field wide mapping post 2018 drills within the block highlighted the sand trend at the Cruse level is in a WSW-ENE direction and that these sands in northern WD-8 are very narrow with maximum widths ranging between 100 ft – 150 ft. Additionally, it showed that by using a smaller well spacing, wells would encounter different producing sand bodies not seen in adjacent wells. Differences in the sand character between wells in the Southern part of the block to wells in the northern part of the block at the Lower Cruse level were also seen. The Lower Cruse section in the southern part of the WD-8 block tends to have thick stacked slope channel sand deposits, while the northern part of WD-8 has relatively thin stacked slope/base of slope channel deposits. Structurally, the presence of an ENE-WSW fault which separates the southern wells from the northern wells was also revealed. Abnormal stratigraphy was also found in Northern WD-8 where the Eocene Navet formation was encountered below the Late Miocene Lower Cruse formation. Two (2) wells in the northern portion of the block found the Navet formation resistive with only one well testing this reservoir. This then presents a new under exploited target reservoir with the block. Mapping of the Navet Formation indicates that this reservoir trends in a WSW-ENE direction. This updated geological model for the WD-8 block resulted in six infill developmental wells being identified to further exploit the remaining reserves within the Lower Cruse and Navet Formations in the WD-8 block.
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