首页> 外文会议>Annual Indonesian Petroleum Association convention and exhibition;Indonesian Petroleum Association convention and exhibition >BERAI CARBONATE DEBRIS FLOW AS RESERVOIR IN THE RUBY FIELD, SEBUKU BLOCK, MAKASSAR STRAITS: A NEW EXPLORATION PLAY IN INDONESIA
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BERAI CARBONATE DEBRIS FLOW AS RESERVOIR IN THE RUBY FIELD, SEBUKU BLOCK, MAKASSAR STRAITS: A NEW EXPLORATION PLAY IN INDONESIA

机译:贝加尔碳酸盐岩碎屑流作为储层在马卡萨斯海峡塞布库区块红宝石油田:印度尼西亚的一项新勘探活动

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Most of the productive carbonate reservoirs in Indonesia are shallow water, high energy carbonate banks and reefal build-ups. The main porosity development in these reservoirs was developed by sea level fluctuations that generated secondary porosity. However, the reservoir in the Ruby Field, Sebuku Block, South Makassar, was deposited under very different conditions and is a good example of a less well known carbonate play type.The Oligo-Miocene Berai Limestone in the Ruby Field consists of re-deposited carbonate located on the outer slope of a large carbonate platform, which has been folded into a structural trap. The limestone clasts range from pebble-size to boulders within a matrix of lime mud and fine abraded bioclasts. The transported packstone and wackestone clasts contain diverse bioclasts that originated in shallow water, mixed epi-reefal and back-reefal environments. The reefal limestone was subject to erosion and re-deposition in a fore-reef toe of slope environment as a debris flow fan, recognizable on seismic. The pore system is contained in both the clasts and matrix, and is enhanced by fractures associated with the folding. Porosity in both the transported clasts and matrix is mostly mouldic and vuggy, resulting mostly from dissolution of foraminifera and red algae after transportation, although some pre-transportation porosity also survives.The carbonate in the Ruby Field has proven to be of good reservoir quality in the Makassar Straits-1 (MKS-1), Makassar Straits-3 (MKS-3) and Makassar Straits-4 (MKS-4) wells, but of lower quality in the Makassar Straits-2 (MKS-2) which can be seen on seismic to be the only well thatpenetrated carbonate between fan-lobes. Excluding MKS-2, these wells penetrated 288-330 feet gross carbonate with net pay between 122-279 feet, with average porosities between 15-17%. MKS-3 well flowed 39 MMSCFGPD sweet gas during an open-hole test and MKS-4 well flowed 39 MMSCFGPD combined from two cased hole tests.
机译:印度尼西亚大多数可生产的碳酸盐储层是浅水,高能碳酸盐库和礁石堆积物。这些储层的主要孔隙度发育是由产生次生孔隙度的海平面波动引起的。然而,位于南孟加锡市Sebuku区块的Ruby油田的储层是在非常不同的条件下沉积的,这是鲜为人知的碳酸盐岩层型的一个很好的例子。 红宝石油田中的中新世Berai石灰岩由重沉积的碳酸盐组成,该碳酸盐位于大型碳酸盐台地的外坡上,已被折叠成一个构造圈闭。石灰石碎屑的范围从卵石大小到石灰泥和细碎生物碎屑基质中的巨石。运输的堆积岩和威克石碎屑含有多种生物碎屑,这些碎屑起源于浅水区,上礁和后礁的混合环境。珊瑚礁石灰岩在斜坡环境的前礁脚趾处作为泥石流扇受到侵蚀和重新沉积,在地震中是可识别的。孔隙系统既包含在碎屑中,也包含在基质中,并且由于与折叠有关的断裂而增强。尽管运输前的多孔性也能幸存,但运输的碎屑和基质中的孔隙度大多是发霉的和弯曲的,这主要是由于运输后有孔虫和红藻的溶解造成的。 在望加锡海峡1(MKS-1),望加锡海峡3(MKS-3)和望加锡海峡4(MKS-4)井中,红宝石油田的碳酸盐被证明具有良好的储层质量,但较低望加锡海峡2号(MKS-2)的质量在地震上是唯一的 在扇形叶之间渗透碳酸盐。除MKS-2井外,这些井均渗透了288-330英尺的碳酸盐岩,净产气量在122-279英尺之间,平均孔隙度在15-17%之间。在两次裸眼测试中,MKS-3井流了39个MMSCFGPD甜味气,MKS-4井流了39个MMSCFGPD的甜味气。

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