首页> 外文会议>Indonesian Petroleum Association Annual Convention v.1; 20031014-20031016; Jakarta; ID >PALEOZOIC AND MESOZOIC PETROLEUM SYSTEMS IN THE TIMOR AND ARAFURA SEAS, EASTERN INDONESIA
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PALEOZOIC AND MESOZOIC PETROLEUM SYSTEMS IN THE TIMOR AND ARAFURA SEAS, EASTERN INDONESIA

机译:印度尼西亚东帝汶和阿拉法拉海地区的古生代和中生代石油系统

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The Timor and Arafura Seas extend over a substantial portion of the northern Australian continental margin. Exploration commenced in Australian waters in 1971, resulting in the discovery of the Greater Sunrise discovery and Evans Shoals gas accumulations, while the first significant discovery in Indonesian waters was the Abadi-1 gas discovery in 2000. The subject of this paper is the interpretation of a new seismic survey, the Matahari MC2D seismic survey, which links the Australian gas discoveries of Greater Sunrise and Evans Shoal with the Abadi accumulation and extends into open acreage within Indonesian waters to the north and east of Abadi. Abadi and earlier Australian discoveries including Greater Sunrise, Evans Shoal and Lynedoch lie on the Sahul Platform, a peri-rift basement high, separated from the Australian craton by a failed Jurassic to Early Cretaceous rift. This rift is identified as the Malita Graben which extends east into the Calder Graben, providing key depocentres and an effective charge kitchen from mature Early to Middle Jurassic Plover Formation source rocks (mixed Type 2 to Type 3 kerogens), which are regarded as the origin of these gas-condensate accumulations. The latter are reservoired in Plover Formation paralic and shelfal sandstones. To the north and northeast of the Abadi discovery, in open acreage, new seismic interpretation has revealed the existence of hitherto untested Paleozoic basins, especially on the southeastern margin of the Tanimbar Trough. Based on analogues with the Bonaparte Basin and Goulburn Graben of northern Australia, these Paleozoic Basins could contain high quality and mature oil-prone source rocks of Cambrian, Devonian and Carboniferous age. In addition, deeply buried Early Cretaceous source rocks may exist along the flanks of the Tanimbar Trough, with similar attributes to excellent quality Echuca Shoals Formation source rocks in the northern Bonaparte Basin, which charged oil discoveries such as the Elang Field in the East Timor Joint Development Area.
机译:帝汶海和阿拉法拉海遍及澳大利亚北部大陆边缘的大部分地区。勘探于1971年在澳大利亚水域开始,从而发现了大日出发现和Evans Shoals气藏,而印度尼西亚水域中的第一个重要发现是2000年的Abadi-1天然气发现。一项新的地震勘探,即Matahari MC2D地震勘探,将澳大利亚在大日出和埃文斯浅滩的天然气发现与Abadi储藏联系起来,并延伸至Abadi北部和东部的印度尼西亚水域内的开放区域。阿巴迪(Abadi)和早期的澳大利亚发现,包括大日出(Sunrise),埃文斯沙(Evans Shoal)和雷尼多克(Lynedoch),位于裂谷周围地下高处的萨胡尔平台(Sahul Platform)上,与侏罗纪至白垩纪早期裂谷的裂隙分开,与澳大利亚克拉通分开。该裂谷被认为是Malita Graben,向东延伸至Calder Graben,提供了重要的沉积中心和从成熟的早侏罗世至中侏罗纪珩科岩层烃源岩(2型至3型混合干酪根)的有效装料厨房。这些气体冷凝物的累积。后者被储存在Plover组的顺层和陆相砂岩中。在阿巴迪发现的北部和东北部,在空地上,新的地震解释揭示了迄今未经测试的古生代盆地的存在,特别是在坦尼巴海槽的东南边缘。基于与澳大利亚北部的Bonaparte盆地和Goulburn Graben的类似物,这些古生代盆地可以包含高质量的,成熟的,易生油的寒武纪,泥盆纪和石炭纪的烃源岩。此外,在Tanimbar槽的两侧可能存在深埋的早白垩纪烃源岩,其相似属性与北波拿巴盆地北部优质的Echuca浅滩组烃源岩相似,这些岩石充有东帝汶联合地的Elang油田等石油发现开发区。

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