首页> 外文会议>Annual Indonesian Petroleum Association convention and exhibition;Indonesian Petroleum Association convention and exhibition >INTRA-ARC TRANS-TENSION DUPLEX OF MAJALENGKA TO BANYUMAS AREA : PROLIFIC PETROLEUM SEEPS AND OPPORTUNITIES IN WEST-CENTRAL JAVA BORDER
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INTRA-ARC TRANS-TENSION DUPLEX OF MAJALENGKA TO BANYUMAS AREA : PROLIFIC PETROLEUM SEEPS AND OPPORTUNITIES IN WEST-CENTRAL JAVA BORDER

机译:马加伦卡至波摩尼亚斯地区的弧内拉伸双峰:爪哇西部中部多产的石油渗漏和机会

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Intra-arc region of Java from Majalengka to Banyumas area straddles the West-Central Java border. The area has been the least-explored area in Java. This contrasts with the facts that numerous petroleum seeps and the first exploration well of Indonesia (Maja-1 well, drilled in 1871, oil discovery) are located in this area. In this study, analyses and synthesis of a series of data comprising gravity, surface geological maps, field study, seismic, and wells lead to a new look of petroleum geology of the area.Major NW-SE trending dextral fault called the Pamanukan-Cilacap Fault Zone crossed this area possibly since the early Neogene or could be slightly older. Around the Majalengka-Kuningan-Majenang areas, the fault zone formed duplex system causing pull-apart opening of trough or trans-tension duplex. The opening controlled the occurrences of pre-Late Miocene back-arc volcanism sourcing the Late Miocene-aged turbiditic Halang volcanoclastic deposits. The Majalengka-Banyumas trough was then inverted in the Mio-Pliocene forming a structural high. Pemali sediments were deposited afterward in low areas flanking the structural high.Trough and trans-tension duplex of the Majalengka-Banyumas area and their inversion had controlled petroleum system of this intra-arc region. High heatflow and geothermal gradient due to pull-apart opening and volcanism, thrust loading within inverted Halang deposits and thick Pemali burial sediments had matured the Paleogene and/or Neogene source rocks existing in this area. Petroleum was generated and migrated updip to Majalengka-Banyumas structural high and trapped in various structures. Numerous oil and gas seeps reveal that petroleum system is working in this area.Reservoir quality, trap integration and poor structure imaging due to volcanic cover may risk exploration. However, based on its active petroleum system, the area merits further exploration endeavor.
机译:从Majalengka到Banyumas地区的Java弧内地区横跨Java中西部边界。该区域是Java中开发最少的区域。与此形成鲜明对比的是,该地区有大量的石油渗漏和印度尼西亚的第一口勘探井(Maja-1井,于1871年钻探,发现了石油)。在这项研究中,对包括重力,地表地质图,野外研究,地震和油井在内的一系列数据的分析和综合,使该地区的石油地质学焕然一新。 NW-SE趋势严重的右旋断层称为Pamanukan-Cilacap断裂带,可能是在新近纪早期或稍早时就越过了该区域。在Majalengka-Kuningan-Majenang地区周围,断层带形成了双相系统,造成槽或超张力双相拉开。该开口控制了中新世晚期弧后火山喷发源于中新世晚期的湍流哈朗火山碎屑沉积物的发生。然后,在Mio-上新世将Majalengka-Banyumas谷倒置,形成结构性高点。之后,Pemali沉积物沉积在结构高地两侧的低洼区域。 Majalengka-Banyumas地区的槽和跨张双相及其反转已控制了该弧内区域的石油系统。由于拉开的开口和火山作用,高热流和地热梯度,倒置的哈朗矿床内的推力载荷和厚厚的佩马利墓葬沉积物使该地区存在的古近系和/或新近系烃源岩成熟。产生了石油并将其上倾向上迁移到Majalengka-Banyumas的构造高处,并被困在各种构造中。大量的石油和天然气渗漏表明该地区正在运行石油系统。 由于火山覆盖而导致的储层质量,圈闭整合和结构成像不良可能有勘探风险。然而,基于其活跃的石油系统,该地区值得进一步勘探。

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