首页> 外文会议>the Indonesian Petroleum Association Annual Convention >COMBINED DIVING WAVE REFRACTION TOMOGRAPHY AND REFLECTION TOMOGRAPHY FOR PSDM VELOCITY MODEL BUILDING (BEKAPAI FIELD, INDONESIA)
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COMBINED DIVING WAVE REFRACTION TOMOGRAPHY AND REFLECTION TOMOGRAPHY FOR PSDM VELOCITY MODEL BUILDING (BEKAPAI FIELD, INDONESIA)

机译:PSDM速度模型建筑的组合潜水波折射断层扫描和反射断层扫描(Bekapai Field,印度尼西亚)

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The offshore Mahakam Delta is well-known for its gas pockets trapped at shallow depth (<400 meters), causing severe degradation of the seismic image. They absorb strongly the seismic energy and lower significantly the signal to noise ratio. Building a reliable velocity model in such areas with short wavelength lateral and vertical velocity variations can be a serious issue. In the Bekapai Field, velocity model building also has to deal with the lack of near angle information in shallow depths as well as weak transmitted signals in deeper intervals.In our case, the velocity model building process combined both a diving wave refraction tomography for shallow intervals (< 400 meters, approximately 1/6 of the streamer cable length) and a reflection tomography for deeper intervals. In this paper, it is shown that diving wave tomography is a robust technique that improves the near surface model. To complete the model for depths greater than 400 meters, the available pre-stack time migration velocity field was combined to the shallow velocity model. The initial velocity field has been further updated with iterative Pre-Stack Depth Migration (PSDM) and reflection tomography with input data having sufficient offset range.The Bekapai final velocity model has enabled a far better focusing of shallow events, including shallow gas amplitude anomalies that were hidden after the 2002 time data-reprocessing. The apparent lateral extension of the anomalies has helped to optimize the design of the upcoming 3D OBC survey on the field. While the diving wave refraction tomography has been suitable for shallow intervals, the reflection tomography has also produced an improved velocity model, contributing to an enhanced focusing ofseismic events and fault planes that enables the interpreter to reduce significantly the remaining structural uncertainty and to deliver reliable structural interpretations for further reservoir model building and field production optimization.
机译:离岸Mahakam Delta以其陷入浅深度(<400米)的气体口袋而闻名,导致地震图像的严重降解。它们强烈地吸收地震能量,显着降低了信噪比。在具有短波长横向和垂直速度变化的这些区域中构建可靠的速度模型可能是一个严重的问题。在Bekapai领域,速度模型建筑也必须处理浅层深度的近角度信息以及更深间隔的弱传输信号。在我们的情况下,速度模型建筑过程组合潜水波折射断层扫描间隔(<400米,拖缆电缆长度的约1/6)和用于更深间隔的反射断层扫描。在本文中,示出了潜水波断层扫描是一种改善近表面模型的稳健技术。为了完成大于400米的深度模型,可用的预堆叠时间迁移速度场将其组合到浅速度模型。初始速度场进一步利用迭代预堆叠深度迁移(PSDM)和反射断层扫描以及具有足够偏移范围的输入数据进行了进一步更新。Bekapai最终速度模型使得能够更好地聚焦浅事件,包括浅气体幅度异常在2002年时间重新处理后被隐藏。异常的表观横向延伸有助于优化即将到来的3D OBC调查的设计。虽然潜水波折射断层扫描是适用于浅间隔的,但反射断层扫描也产生了一种改进的速度模型,有助于增强的对抗血液事件和故障平面,使得口译员能够显着降低剩余的结构性不确定性并提供可靠的结构进一步储层模型建设和现场生产优化的解释。

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