首页> 外文会议>the Indonesian Petroleum Association Annual Convention >SEQUENCE STRATIGRAPHIC CORRELATION AND SEDIMENTOLOGICAL IMPLICATIONS, EAST JAVA BASIN: COMPARISONS AND LESSONS LEARNED FROM OUTCROP ANDSUBSURFACE STUDIES
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SEQUENCE STRATIGRAPHIC CORRELATION AND SEDIMENTOLOGICAL IMPLICATIONS, EAST JAVA BASIN: COMPARISONS AND LESSONS LEARNED FROM OUTCROP ANDSUBSURFACE STUDIES

机译:序列地层相关和沉积物意义,东爪哇盆地:从露头和对手研究中吸取的比较和经验教训

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ExxonMobil Indonesia has been conducting field trips to East Java to honor the memory of Ted Apotria, a colleague that passed away in 2009. The field trips include visits to the Rembang and Kendeng Zones and compare the stratigraphic and tectonic observations of the outcrop areas to the subsurface in the Cepu area. Through discussions with field trip participants from both the geosciences and engineering disciplines, a new stratigraphic framework was developed in the East Java Basin to correlate between the Oligocene-Miocene outcrops in the Rembang Hills to subsurface core and seismic data in the onshore Cepu Block. Outcrop exposures have been regionally correlated to sub-surface well and seismic data sets constrained by biostratigraphic and strontium isotope age control. The subsurface also provides further control for the older part of the Tertiary stratigraphy not exposed in outcrops.The stratigraphy of the outcrop and subsurface locations record the interplay between tectonics, sediment supply and reservoir quality during the evolution of the East Java Basin. This provides important control for understanding the timing of clastic influx and the effect on the distribution of carbonate rocks and reservoirs because the multiple producing intervals reside in the two lithologies (carbonates and sandstones) and are bounded by seals of different ages and lithologies. A detailed understanding of the stratigraphic evolution of sandstone and carbonate prone intervals has beenessential to efficient exploration and production of natural resources within the complicated tectono-stratigraphic setting of the East Java Basin.
机译:埃克森美孚印度尼西亚一直在开展东爪哇省的野外旅行,以纪念2009年通过的同事们纪念Ted Apotria。实地旅行包括访问Rembang和Kendeng区,并比较露头区域的地层和构造观察地产在CEPU区域。通过讨论地球科学和工程学科的实地旅行参与者,东爪哇盆地开发了一种新的地层框架,以与陆上CEPU块中的剩余核心和地震数据之间的寡茂 - 中世界露头之间相关联。露出露天暴露于区域相关与由生物数据井和锶同位素年龄控制受到的子表面阱和地震数据集。地下还为露头暴露的三级地层的较旧部分提供了进一步的控制。露头和地下位置的地层记录了东爪哇盆地进化期间构造,沉积物供应和水库质量之间的相互作用。这提供了对理解碎片流入的时间的重要控制和对碳酸盐岩和储层分布的影响,因为多种产生间隔位于两个岩性(碳酸盐和砂岩)中,并且由不同年龄和岩石的密封界界定。详细了解砂岩的地层演变和碳酸盐酸的间隔已绝佳以高效的探索和生产东爪哇盆地复杂的构造 - 地层环境中的自然资源。

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