首页> 外文会议>Indonesian Petroleum Association Annual Convention v.1; 20031014-20031016; Jakarta; ID >THE COLLISION OF THE EAST JAVA MICROPLATE AND ITS IMPLICATION FOR HYDROCARBON OCCURRENCES IN THE EAST JAVA BASIN
【24h】

THE COLLISION OF THE EAST JAVA MICROPLATE AND ITS IMPLICATION FOR HYDROCARBON OCCURRENCES IN THE EAST JAVA BASIN

机译:东爪哇盆地的三叠纪碰撞及其对油气发生的启示

获取原文
获取原文并翻译 | 示例

摘要

The East Java basin is one of the major petroliferous basins in Indonesia. However, understanding of the tectonic development of the area is still subject to ongoing debate. Detailed regional geologic investigation was carried out to study and evaluate tectonic history and basin development in relation to hydrocarbon potential of the area. Recently acquired seismic data and hydrocarbon discovery in the sandstone unit of the Ngimbang Fm. in the EJ-1 well at East Java triggered a new interpretation of tectonism and basin development, especially during Paleogene time. From the end of Cretaceous to Early Eocene, a continental fragment, possibly detached from the Gondwana super-continent to the south, drifted northeastward approaching the Late Cretaceous to early Tertiary subduction complex (Lok Ulo-Meratus belt). The collision of this micro-continent with the eastern margin of the Sunda Microplate caused the Eocene magmatic activity to cease and uplifted the subduction complex, creating the Meratus Mountains in the eastern part of Kalimantan and The Lok Ulo melange complex in the central Java. The grain of the continental basement influenced basin trends. In eastern part of East Java Basin the dominant basement grain is E-W, as can be particularly well observed controlling the Kendeng and Madura Troughs. At the very close of this period, compressional tectonism due to the northward convergence between the Australian plate and the Sundaland margin reactivated these pre-existing E-W basement faults into strike-slip movement (e.g. along the Sakala Fault Zone). Another type of basin configuration developed at the collision zone oriented NE-SW, parallel to the direction of the collisional suture along Lok Ulo - Meratus Complexes. As a result, it is proposed that the Muria Trough in the north is a foreland basin which probably can be traced further south through Kendal Sub-basin to Kebumen Sub-basin. The result of this study reveals a new target for hydrocarbon exploration in the area.
机译:东爪哇盆地是印度尼西亚主要的含油盆地之一。然而,对这一地区构造发展的了解仍在进行中。进行了详细的区域地质调查,以研究和评估与该地区油气潜力有关的构造历史和盆地发育。 Ngimbang Fm砂岩单元中最近获得的地震数据和油气发现。东爪哇省EJ-1井的地震触发了对构造和盆地发育的新解释,特别是在古近纪时期。从白垩纪末期到始新世,大陆碎片可能从冈瓦纳超大陆分离到南部,向东北漂移,到达白垩纪晚期到第三纪俯冲复合体(Lok Ulo-Meratus带)。该微大陆与Sun他微板块东缘的碰撞导致始新世岩浆活动停止并抬升了俯冲带,形成了加里曼丹东部的梅拉图斯山脉和爪哇中部的洛乌洛混杂体。大陆基底的颗粒影响了盆地的趋势。在东爪哇盆地东部,主要的基底晶粒是E-W,可以很好地观察到控制肯登和马杜拉海槽。在这一时期的最后阶段,由于澳大利亚板块和桑达兰边缘之间的北向汇合而产生的压缩构造作用使这些先前存在的E-W基底断层重新激活为走滑运动(例如沿着Sakala断裂带)。在面向碰撞区的NE-SW处开发的另一种盆地构造,与沿Lok Ulo-Meratus Complexs的碰撞缝合线方向平行。因此,建议北部的穆里亚海槽是前陆盆地,可能可以通过肯德尔次盆地到克布门次盆地进一步向南追溯。这项研究的结果揭示了该地区油气勘探的新目标。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 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