首页> 外文期刊>Marine and Petroleum Geology >Linking the influence of diagenetic properties and clay texture on reservoir quality in sandstones from NW Borneo
【24h】

Linking the influence of diagenetic properties and clay texture on reservoir quality in sandstones from NW Borneo

机译:与NW婆罗洲砂岩中砂岩储层质量的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Reservoir studies in the Sandakan sub-basin NW Borneo are challenging and inexplicable due to complex diagenetic effects such as compaction, cementation, dissolution and depositional means including grain size, sorting and packing with reference to clay texture. These diagenetic effects together impart significant amounts of uncertainty on reservoir quality assessment. In this regard, we documented the mineralogical, diagenetic and reservoir properties of sandstones from the Sandakan Formation, NW Borneo through thin sections, SEM, XRD, XRF, He-porosimeter and poroperm. In order to analyze the influential parameters, we used matrix, grain rearrangement and clay coating around detrital grains for the reservoir quality. Our results show that the sub-litharenites to quartz arenite that dominate in the sandstones are drawn from recycled orogenic sand. Furthermore, reservoir properties of the sandstones were ascertained to be controlled by diagenesis, micro quartz with clay coatings and pressure dissolution of feldspar with the alteration of lithic fragments. The result shows that the physical compaction, rearrangements and ductility of grains were the reasons that reduced porosity and permeability. The main reason for porosity reduction in the present study is pressure dissolution that resulted in the form of chemical compaction induced by micas with grain contacts. Nonetheless, through SEM and petrography, clay coatings around the grains and dissolution of feldspar were found to optimally contribute to the preservation of reservoir properties. Dissolution of feldspar and kaolinization resulted in the formation of secondary porosity that allows meteoric water to percolate through the open and detachment spaces of quartz or other grains. This percolation is also responsible in enhancing the pore throat radii in the reservoir media of the analyzed sandstones. These traits are obliging to diagenetic effects on porosity and permeability, which are linked with the physical compaction and clays coating to reduce and preserve the reservoir properties respectively of same type of reservoirs globally.
机译:施达坎亚盆地NW Bordeo的储层研究是挑战性,并且由于复杂的成岩作用,例如压实,胶泥化,溶解和沉积方法,包括晶粒尺寸,分选和包装参考粘土纹理。这些成岩效应在一起赋予储层质量评估的大量不确定性。在这方面,我们记录了来自Sandakan Chormation的砂岩的矿物学,成岩性和储层和储层性质,通过薄段,SEM,XRD,XRF,He-孔孔计和茯苓。为了分析有影响力的参数,我们使用碎屑颗粒周围的碎屑颗粒矩阵,谷物重排和粘土涂层。我们的研究结果表明,石英植物在砂岩中占据砂岩中的石英砷,从再循环的造山床中汲取。此外,确定砂岩的储层性质,以通过成岩作用,微石英,具有粘土涂层的微石英和具有锂碎片的改变的粘土涂层和压力溶解。结果表明,晶粒的物理压实,重排和延展性是降低孔隙率和渗透性的原因。本研究中孔隙率降低的主要原因是压力溶解,其导致由晶粒触点诱导的化学压实形式。尽管如此,通过SEM和岩画,发现晶粒周围的粘土涂层和长石的溶解将最佳地有助于保存储层性质。长石和高岭化的溶解导致形成二次孔隙率,使得迁移水通过石英或其他晶粒的开放和分离空间来渗滤。这种渗透性也负责增强分析的砂岩的储层介质中的孔喉半径。这些性状涉及对孔隙率和渗透性的成岩效应,其与物理压实和粘土涂层连接,以减少并保留全球相同类型的储层的储层性质。

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