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Formation, distribution, resource potential, and discovery of Sinian–Cambrian giant gas field, Sichuan Basin, SW China

机译:中国四川盆地震旦纪-寒武纪巨型气田的形成,分布,资源潜力和发现

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The Anyue Sinian–Cambrian giant gas field was discovered in central paleo-uplift in the Sichuan Basin in 2013, which is a structural-lithological gas reservoir, with 779.9 km2proven gas-bearing area and 4 403.8×108m3proven geological reserves in the Cambrian Longwangmiao Formation in Moxi Block, and the discovery implies it possesses trillion-cubic-meter reserves in the Sinian. Cambrian Formations in Sichuan Basin. The main understandings achieved are as follows: (1) Sinian–Cambrian sedimentary filling sequences and division evidence are redetermined; (2) During Late Sinian and Early Cambrian, “Deyang–Anyue” paleo-taphrogenic trough was successively developed and controlled the distribution of source rocks in the Lower-Cambrian, characterized by 20–160 m source rock thickness,TOC1.7%–3.6% andRo2.0%–3.5%; (3) Carbonate edge platform occurred in the Sinian Dengying Formation, and carbonate gentle slope platform occurred in the Longwangmiao Formation, with large-scale grain beach near the synsedimentary paleo- uplift; (4) Two types of gas-bearing reservoir, i.e. carbonate fracture-vug type in the Sinian Dengying Formation and dolomite pore type in the Cambrian Longwangmiao Formation, and superposition transformation of penecontemporaneous dolomitization and supergene karst formed high porosity-permeability reservoirs, with 3%–4% porosity and (1–6)×10?3μm2permeability in the Sinian Dengying Formation, and 4%–5% porosity and (1–5)×10?3μm2permeability in the Cambrian Longwangmiao Formation; (5) Large paleo-oil pool occurred in the core of the paleo-uplift during late Hercynian—Indosinian, with over 5 000 km2and (48–63)×108t oil resources, and then in the Yanshanian period, in-situ crude oil cracked to generate gas and dispersive liquid hydrocarbons in deep slope cracked to generate gas, both of which provide sufficient gas for the giant gas field; (6) The formation and retention of the giant gas field is mainly controlled by paleo-taphrogenic trough, paleo-platform, paleo-oil pool cracking gas and paleo-uplift jointly; (7) Total gas resources of the Sinian–Cambrian giant gas field are preliminarily predicted to be about 5×1012m3, and the paleo-uplift and its slope, southern Sichuan Basin depression and deep formations of the high and steep structure belt in east Sichuan, are key exploration plays. The discovery of deep Anyue Sinian–Cambrian giant primay oil-cracking gas field in the Sichuan Basin, is the first in global ancient strata exploration, which is of great inspiration for extension of oil & gas discoveries for global middle-deep formations from Lower Paleozoic to Middle–Upper Proterozoic strata.
机译:2013年,四川盆地中部古隆起发现安岳震旦纪—寒武纪巨型气田,为构造岩性气藏,含气面积779.9 km2,寒武纪龙王庙组探明地质储量4 403.8×108m3。该发现表明它在震旦纪拥有兆兆立方米的储量。四川盆地寒武系地层。取得的主要理解如下:(1)重新确定震旦—寒武纪沉积充填序列和划分证据; (2)在震旦纪晚期和寒武纪早期,相继开发了“德阳—安岳”古成槽,并控制了下寒武统的烃源岩分布,其特征是烃源岩厚度为20〜160 m,TOC为1.7%〜 3.6%和Ro2.0%–3.5%; (3)震旦系灯影组有碳酸盐岩边缘台地,龙王庙组有碳酸盐岩缓坡台地,在同沉积古隆起附近有大型的粮滩。 (4)震旦系灯影组碳酸盐岩缝洞型和寒武纪龙王庙组白云岩孔隙型两种含气储层,准时白云石化和表生岩溶的叠置转化形成高孔隙度渗透率储层,3震旦系灯影组孔隙度为%–4%,渗透率为(1-6)×10?3μm2;寒武纪龙王庙组孔隙度为(4%–5%)孔隙率(1–5)×10?3μm2; (5)海西—印支期晚期古隆起的核心部位有大量古油藏,储量超过5000 km2,(48〜63)×108t石油资源,燕山时期则为原位原油。裂化产生气体,深层斜坡中的分散液态烃裂化产生气体,两者都为巨大的气田提供了足够的气体; (6)巨型气田的形成和保留主要受古成藏槽,古平台,古油藏裂解气和古隆起共同控制; (7)初步预测震旦—寒武统巨型气田的天然气资源总量约为5×1012m3,古隆起及其斜坡,四川盆地南部凹陷和川东高陡构造带的深部地层,是关键的探索剧本。四川盆地深层的安岳震旦纪-寒武纪巨型原始石油裂解气田的发现,是全球古代地层勘探中的第一个领域,这对将油气发现扩展到下古生界的全球中深层地层具有重大启示到中上元古界地层。

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