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STRUCTURAL STYLES AND PETROLEUM SYSTEM MODELLING OF THE NORTH MAKASSAR STRAITS, INDONESIA

机译:印度尼西亚北麦克萨斯峡地峡的结构风格和石油系统建模

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The northern Makassar Straits lies within the offshore portion of the Kutai Basin, a very prolific petroleum province of Central Indonesia. Within this Basin, GDF SUEZ EPI has interests in Muara Bakau and North Ganal exploration licenses and is looking at opportunities to expand its portfolio in Indonesia. As part of a regional review of the northern Makassar Basin, an integrated study was undertaken to detail the tectonic evolution and remaining hydrocarbon potential of the area. The study uses the interpretation of speculative 2D seismic lines, 2D basin modelling and well data. The results of our study demonstrate that the northern Makassar Basin initiated with a rifting of Middle Eocene to Early Oligocene age. This resulted in the development of a number of basement faults oriented NNW-SSE and organized in an en-echelon pattern. At the same time, a proto- delta of the Mahakam River seems to have developed southwards of its present-day location. Northwest/southeast trending compression started in Middle Miocene and continued until the present day. Basin inversion and uplift were generated, together with faults reactivation and development of broad anticlines within the basement. Fault inversion was prominent in the relay ramps and accommodation zones occurred in between the en- echelon basement faults. Thick-skinned tectonics were coupled with a thin- skinned deformation initiated within the overlying sediments of the Mahakam Delta progradation system. This led to the development of extensional growth faults near the shelf break and toe-thrusts associated with tight and asymmetric folds. Progressive compression, while delta progradation continued, produced reactivation of the extensional growth faults and further uplift of the anticlines. The results of our structural study were then used as input for 2D basin modeling which allowed us to improve our understanding of the regional petroleum system and assess potential opportunities within this area.
机译:北·帕萨萨尔海峡位于印度尼西亚中部近景石油省的Kutai盆地的近海部分。在这个盆地内,GDF Suez EPI在Muara Bakau和北甘农勘探许可证中兴趣,并正在观察扩大印度尼西亚投资组合的机会。作为北马卡萨尔盆地的区域审查的一部分,综合研究是为了详细说明该地区的构造演化和剩余的碳氢化合物潜力。该研究采用了推测性2D地震线,2D盆地建模和井数据的解释。我们的研究结果表明,北幼儿园盆地发起了中期欧世的脱水至早期寡核糖年龄。这导致开发许多面向上的NNW-SSE的基底断层,并以en-echelon模式组织。与此同时,Mahakam河的Proto似乎已经开发了本日地点的向南。西北/东南趋势压缩开始于中间内科,并继续直到现今。生成盆地反转和隆起,与地下室内的宽度反射和开发的故障一起产生。在继电器坡道和梯田地下室故障之间发生的接收区中发生故障反演。厚皮的构造与在Mahakam Delta促进系统的上覆沉积物内引发的薄皮肤变形。这导致了与紧密和不对称折叠相关的搁板断裂和脚趾伸出的延伸增长故障的发展。渐进式压缩,而Delta促进继续,产生了延伸生长故障的重新激活,并进一步隆起的预防线。然后,我们的结构研究结果被用作2D盆地建模的投入,使我们能够改善我们对区域石油系统的理解,并评估该领域内的潜在机会。

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