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Depositional environments and source rock investigations of the Oligocene to Middle Miocene deposits in the Ardjuna Basin, offshore Northwest Java, Indonesia.

机译:印度尼西亚西北爪哇近海Ardjuna盆地的渐新世至中新世沉积物的沉积环境和烃源岩调查。

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摘要

Investigations of depositional environments, paleogeographic evolution, source rock potential/maturity, and petroleum generation, expulsion, migration and accumulation were performed on the Oligocene to Middle Miocene deposits in the Ardjuna Basin, offshore Northwest Java, using integrated geologic, seismic and geochemical approaches.;The Oligocene to Middle Miocene sediments were deposited in a generally transgressive sequence. It is the most prospective stratigraphic unit for petroleum exploration in the Ardjuna Basin. The rocks comprise three Formations: Talang Akar, Baturaja and Cibulakan. Talang Akar sediments were deposited in a deltaic to shore environment, Baturaja carbonates were formed on a warm and flat shelf, and Cibulakan sediments were deposited mostly in the inner to outer shelf environment. Paleogeography of six stages within the study interval, showing the degree of marine transgression were mapped based on integrated biostratigraphic, paleoenvironmental, and seismic-stratigraphic data.;The coals and carbonaceous shales deposited in the deltaic and nearshore environment of the Talang Akar Formation are petroleum source rocks for the waxy oils produced in the Ardjuna Basin. The organic matter contains predominantly vitrinite maceral and up to 30% exinite maceral.;Source rock temperature, after calibration with vitrinite reflectance, provides an accurate quantitative measurement for predicting the level of thermal maturation. This compensates for the ambiguity of using depth as maturation indicator, particularly in areas with a wide range of geothermal gradients (2;Two geochemical approaches were used and compared in petroleum resource assessment: petroleum yield (S1) method and genetic potential (S2) method. The oil generative kitchen, the Ardjuna depocenter, has the best opportunity for new oil discovery. This model has since been proved by subsequent drilling leading to several oil discoveries in last two years.
机译:利用综合的地质,地震和地球化学方法,对爪哇西北部阿杜纳盆地中渐新世至中新世的沉积环境,古地理演化,烃源岩的潜力/成熟度以及石油的产生,驱出,运移和聚集进行了调查。 ;中新世至中新世沉积物通常以海侵顺序沉积。它是Ardjuna盆地最有前途的石油勘探地层单元。这些岩石包括三个地层:塔朗阿卡(Talang Akar),巴图拉雅(Baturaja)和西布拉坎(Cibulakan)。塔朗阿卡(Talang Akar)沉积物沉积在三角洲至岸边的环境中,在温暖而平坦的层架上形成了Baturaja碳酸盐,西布拉坎沉积物大部分沉积在了内外层架的环境中。在研究区间内的六个阶段的古地理学,根据综合的生物地层,古环境和地震地层数据绘制了海侵程度,绘制了图谱;沉积在塔朗阿卡组三角洲和近岸环境中的煤和碳质页岩是石油阿尔乔纳盆地(Ardjuna Basin)生产的蜡质油的烃源岩。有机物主要包含辉石质辉石岩和最多30%的辉绿岩辉石岩;在通过镜质岩反射率校准后,源岩温度可提供准确的定量测量值,以预测热成熟度。这弥补了使用深度作为成熟度指标的不确定性,特别是在地热梯度范围较广的地区(2;在石油资源评估中使用了两种地球化学方法并进行了比较:石油产量(S1)方法和遗传潜力(S2)方法。产油厨房Ardjuna储油中心拥有发现新油的最佳机会,此模型已通过随后的钻探得以证明,在最近两年中又发现了几处油。

著录项

  • 作者

    Wu, Chia-Hsin Charlie.;

  • 作者单位

    The University of Texas at Dallas.;

  • 授予单位 The University of Texas at Dallas.;
  • 学科 Geology.;Biogeochemistry.;Geochemistry.
  • 学位 Ph.D.
  • 年度 1991
  • 页码 210 p.
  • 总页数 210
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 康复医学;
  • 关键词

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