Petrophysical Analysis to Determine Reservoir and Source Rocks in Berau Basin, West Papua Waters

Popy Dwi Indriyani, A. Harja, T. B. Nainggolan
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引用次数: 1

Abstract

Berau Basin is assessed to have same potential in clastic sediments with Mesozoic and Paleozoic ages, where reservoirs and source rocks are similar to productive areas of hydrocarbons in Northwest Shield Australia. This study aims to identify the hydrocarbon prospect zones and potential rocks zones using petrophysical parameters, such as shale volume, porosity, water saturation and permeability. Petrophysical analysis of reservoir and source rock are carried out on three wells located in the Berau Basin, namely DI-1, DI-2 and DI-3 in Kembelangan and Tipuma Formation. Qualitative analysis shows that there are 4 reservoir rock zones and 4 source rock zones from thorough analysis of these three wells. Based on quantitative analysis of DI-1 well, it has an average shale volume (Vsh) 9.253%, effective porosity (PHIE) 20.68%, water saturation (Sw) 93.3% and permeability (k) 55.69 mD. DI-2 well’s average shale volume, effective porosity, water saturation and permeability values are 29.16%, 2.97%, 67.9% and 0.05 mD, respectively. In DI-3 well, average shale volume, effective porosity, water saturation and permeability values are 6.205%, 19.36%, 80.2% and 242.05 mD, respectively. From the reservoir zone of these three wells in Kembelangan Formation, there are no show any hydrocarbon prospect.
确定西巴布亚水域贝劳盆地储层和烃源岩的岩石物理分析
贝劳盆地在中生代和古生代的碎屑沉积物中具有相同的潜力,那里的储层和烃源岩与澳大利亚西北地盾的碳氢化合物生产区相似。本研究旨在利用页岩体积、孔隙度、含水饱和度和渗透率等岩石物理参数,确定油气远景区和潜在岩石区。对位于Berau盆地的三口井,即Kembelangan和Tipuma组的DI-1、DI-2和DI-3,进行了储层和烃源岩的岩石物理分析。定性分析表明,通过对这三口井的深入分析,共有4个储集岩带和4个烃源岩带。根据DI-1井的定量分析,其平均页岩体积(Vsh)为9.253%,有效孔隙度(PHIE)为20.68%,含水饱和度(Sw)为93.3%,渗透率(k)为55.69mD。DI-2井的平均页岩体积、有效孔隙度、含水饱和度和渗透率分别为29.16%、2.97%、67.9%和0.05mD。DI-3井的平均页岩体积、有效孔隙度、含水饱和度和渗透率分别为6.205%、19.36%、80.2%和242.05mD。从Kembelangan组这三口井的储层来看,没有任何油气远景。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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