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首页> 外文期刊>Marine and Petroleum Geology >Seismic characteristics of a reef carbonate reservoir and implications for hydrocarbon exploration in deepwater of the Qiongdongnan Basin, northern South China Sea
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Seismic characteristics of a reef carbonate reservoir and implications for hydrocarbon exploration in deepwater of the Qiongdongnan Basin, northern South China Sea

机译:南海北部琼东南盆地深水礁碳酸盐岩储层的地震特征及其对油气勘探的启示

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Our analysis of approximately 40,000 km of multichannel 2-D seismic data, reef oil-field seismic data, and data from several boreholes led to the identification of two areas of reef carbonate reservoirs in deepwater areas (water depth > 500 m) of the Qiongdongnan Basin (QDNB), northern South China Sea. High-resolution sequence stratigraphic analysis revealed that the transgressive and highstand system tracts of the mid-Miocene Meishan Formation in the Beijiao and Ledong-Lingshui Depressions developed reef carbonates. The seismic features of the reef carbonates in these two areas include chaotic bedding, intermittent internal reflections, chaotic or blank reflections, mounded reflections, and apparent amplitude anomalies, similar to the seismic characteristics of the LH11-1 reef reservoir in the Dongsha Uplift and Island Reef of the Salawati Basin, Indonesia, which house large oil fields. The impedance values of reefs in the Beijiao and Ledong-Lingshui Depressions are 8000-9000 g/cc x m/s. Impedance sections reveal that the impedance of the LH11-1 reef reservoir in the northern South China Sea is 8000-10000 g/cc x m/s, whereas that of pure limestone in BD23-1-1 is >10000 g/cc x m/s. The mid-Miocene paleogeography of the Beijiao Depression was dominated by offshore and neritic environments, with only part of the southern Beijiao uplift emergent at that time. The input of terrigenous sediments was relatively minor in this area, meaning that terrigenous source areas were insignificant in terms of the Beijiao Depression; reef carbonates were probably widely distributed throughout the depression, as with the Ledong-Lingshui Depression. The combined geological and geophysical data indicate that shelf margin atolls were well developed in the Beijiao Depression, as in the Ledong-Lingshui Depression where small-scale patch or pinnacle reefs developed. These reef carbonates are promising reservoirs, representing important targets for deepwater hydrocarbon exploration.
机译:我们对大约40,000 km的多通道2-D地震数据,礁石油田地震数据以及来自多个钻孔的数据进行了分析,从而确定了琼东南地区深水区(水深> 500 m)的两个礁岩碳酸盐岩储层区域。南海北部盆地(QDNB)。高分辨率层序地层分析表明,北郊凹陷和乐东-陵水hui陷中新世中山梅山组的海侵和高架系统带发育了碳酸盐碳酸盐岩。这两个地区的碳酸盐碳酸盐岩的地震特征包括混乱的层理,间歇的内部反射,混沌或空白的反射,堆砌的反射以及明显的振幅异常,类似于东沙隆起和孤岛的LH11-1礁岩储层的地震特征。印度尼西亚萨拉瓦蒂盆地的礁石,这里有大型油田。北郊凹陷和乐东-陵水凹陷的礁石阻抗值为8000-9000 g / cc x m / s。阻抗剖面显示,南海北部LH11-1礁岩储层的阻抗为8000-10000 g / cc xm / s,而BD23-1-1中的纯石灰石的阻抗> 10000 g / cc xm / s 。北郊De陷的中新世中期古地理主要由近海和含沙环境控制,当时只有部分北郊隆起发生。在该地区,陆源沉积物的投入相对较小,这意味着从北郊jia陷来看,陆源区是微不足道的。与乐东-陵水hui陷一样,礁碳酸盐岩可能广泛分布于整个the陷。综合的地质和地球物理数据表明,在北郊De陷,陆缘环礁发育良好,在乐东—陵水pression陷,小规模的斑块或石峰礁发育。这些礁碳酸盐岩是很有前途的储层,是深水烃勘探的重要目标。

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