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PALEOZOIC AND MESOZOIC PETROLEUM SYSTEMS IN THE TIMOR AND ARAFURA SEAS, EASTERN INDONESIA

机译:古生代和中生代石油系统在东印度尼西亚东部和阿拉弗拉海

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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:帝和阿拉弗拉海海洋延伸在澳大利亚北部大陆边缘的相当大的部分。探索在澳大利亚水域开始于1971年,导致大日升发现和埃文斯浅滩气藏的发现,而在印尼海域第一显著的发现是在2000年的阿巴迪-1天然气发现这篇文章的主题是解释一个新的地震勘测中,的Matahari MC2D地震勘测,哪个环节大的日出和埃文斯浅滩的澳大利亚天然气的发现与阿巴迪积累和延伸到印尼水域阿巴迪的北部和东部中打开面积。阿巴迪和早期发现澳大利亚的大,包括日出,埃文斯浅滩和Lynedoch谎言Sahul平台上,迫裂谷地下室高,来自澳大利亚克拉通相隔一个失败的侏罗纪 - 早白垩世的裂痕。这种裂痕被识别为Malita地堑其中向东延伸到考尔德地堑,提供主要沉积中心和从成熟早期的有效电荷厨房中侏罗纪船形成源岩(混合类型2到类型3的干酪根),它们被视为原点这些凝析气藏。后者在储集船编队近海和shelfal砂岩。到阿巴迪发现的北部和东北部,在开放面积,新的地震解释透露迄今未测试的古生代盆地的存在,尤其是在Tanimbar槽的东南缘。根据与波拿巴盆地和澳大利亚北部的古尔堑类似物,这些古生代盆地可能含有高品质和成熟的寒武系,泥盆系和石炭系年龄的油源岩。此外,深埋地下的早白垩世烃源岩可以沿着Tanimbar槽的侧面存在的,具有类似属性,以优良的品质伊丘卡浅滩烃源岩在北波拿巴盆地,其充电油田的发现,如饿狼场的东帝汶联合开发区。

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