首页> 外文会议>Annual convention of the indonesian petroleum association >IDENTIFICATION OF BIOGENIC GAS POTENTIAL USING INTEGRATED SEISMIC DATA, WIRELINE LOG AND GEOCHEMISTRY DATA; A STUDY CASE: MURIAH SUB-BASIN, BAWEAN ARC, OFFSHORE NORTHERN EAST JAVA
【24h】

IDENTIFICATION OF BIOGENIC GAS POTENTIAL USING INTEGRATED SEISMIC DATA, WIRELINE LOG AND GEOCHEMISTRY DATA; A STUDY CASE: MURIAH SUB-BASIN, BAWEAN ARC, OFFSHORE NORTHERN EAST JAVA

机译:使用集成地震数据,有线日志和地球化学数据识别生物气体潜力;一项研究案例:穆里亚河盆地,巴瓦恩弧,海上东爪哇省

获取原文

摘要

The research area is located in the sub - basin of the Muriah and Bawean Arc in the offshore area of Northern East Java. Integration of Seismic data, wireline log and geochemistry data are used to determine the main reservoirs in the research area, to know the distribution and accumulation and also to understand the most potential points containing biogenic gases. The result of the research is the main reservoir to be an exploration target is Ngrayong Formation (sandstone) and Kujung 1 Formation (limestone), while genetics of biogenic gas in the research area is formed in Kujung II Formation as a source rock that have temperature at 400 - 700°C with Ro 0.35, which expulsed at last Oligocene and formed in Muriah sub-basin at 800 m below the surface. One of the important things is to find the accumulation point of hydrocarbon accumulation, as evident by the discovery of biogenic gas at KPD wells (> 98% Methane). It can be interpreted that in adjacent areas entering the window of biogenic gas maturity and having coal content and having a low geothermal gradient have had a potential area for biogenic gas that can be developed. The distribution of the biogenic gas is controlled by the NE-SW geological structure, while the accumulation of biogenic gas in addition to the hydrocarbon reservoir factor itself is controlled by hydrocarbon traps located in the research area, such as structural and stratigraphic traps.
机译:研究区位于子 - 的Muriah和巴韦安岛弧盆北东爪哇海域。地震数据,电缆测井和地球化学数据的整合来确定研究区主要水库,要知道分配和积累,也明白含有生物气最有潜力点。该研究的结果是成为一个勘探目标主贮存器Ngrayong组(砂岩)和Kujung 1组(石灰石),而在Kujung II组形成为具有温度源岩在研究领域生物气的遗传学在400 - 700℃下用RO 0.35,这expulsed最后渐并在表面800米以下形成在Muriah次盆地。其中一个重要的事情是由生物气在KPD井发现找到烃积聚的累积点,如明显的(> 98%甲烷)。这可以解释为,在邻近地区进入生物气体成熟的窗口,并有合理的煤矿内容和具有低的地热为生物气可开发的梯度有一个潜在的区域。的生物气的分布由NE-SW地质结构控制的,而生物气的除烃储层因子本身的积累是由位于在研究领域烃陷阱,如结构和地层圈闭控制。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号