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Geology,resource potentials,and properties of emerging and potential China shale gas and shale oil plays

机译:中国页岩气和页岩油产区的地质,资源潜力以及新兴和潜在的属性

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This paper describes the geology of organic-rich shales in China, their resource potentials, and properties of emerging and potential China shale gas and shale oil plays. Marine, lacustrine, and coastal swamp transitional shales were estimated to have the largest technically recoverable shale gas resource (25.08 trillion cubic meters or 886 trillion cubic feet) and 25 to 50 billion barrels of technically recoverable shale oil resource. The Precambrian Sinian Doushantuo Formation to Silurian Longmaxi black marine shales mainly accumulated in the intrashelf low to slope environments in the Yangtze Platform in South China and in the Tarim Platform in northwest China. The marine shales in the Yangtze Platform have high maturity (Ro of 1.3%-5%), high total organic carbon (mainly >2%),high brittle-mineral content, and have been identified as emerging shale gas plays. The Lower Paleozoic marine shales in the Upper Yangtze area have the largest shale gas potential and currently top the list as exploration targets. The Carboniferous to Permian shales associated with coal and sandstones were mainly formed in transitional depositional settings in north China, northwest China, and the Yangtze Platform in south China. These transitional shales are generally rich in clay with a medium level of shale gas potential. The Middle Permian to Cenozoic organic-rich lacustrine shales interbedded with thin sandstone and carbonate beds are sporadically distributed in rifted basins across China. Their main potentials are as hybrid plays (tight and shale oil). China shales are heterogeneous across time and space, and high-quality shale reservoirs are usually positioned within transgressive systems tract to early highstand systems tract intervals that were deposited in an anoxic depositional setting. For China's shale plays, tectonic movements have affected and disrupted the early oil and gas accumulation, making tectonically stable areas more favorable prospects for the exploration and development of shale plays.
机译:本文介绍了中国富含有机物的页岩的地质,其资源潜力以及新兴的和潜在的中国页岩气和页岩油产区的性质。据估计,海洋,湖泊和沿海沼泽过渡性页岩拥有技术上可开采的最大页岩气资源(25.08万亿立方米或886万亿立方英尺)和25至500亿桶技术可开采的页岩油资源。前寒武纪震旦系杜沙托组至志留系龙马溪黑色海相页岩主要聚集在华南扬子台地和西北塔里木台地的低层至斜坡内环境中。扬子平台的海相页岩具有较高的成熟度(Ro为1.3%-5%),有机碳总量较高(主要是> 2%),高的脆性矿物含量,被确定为新兴的页岩气气藏。扬子江上游地区的下古生界海相页岩具有最大的页岩气潜力,目前是勘探目标中的首位。与煤和砂岩有关的石炭纪至二叠纪页岩主要形成于华北,西北和华南扬子平台的过渡沉积环境中。这些过渡页岩通常富含粘土,具有中等水平的页岩气潜力。中二叠纪至新生代富含有机质的湖相页岩与薄层砂岩和碳酸盐岩床交错分布在整个裂谷盆地中。它们的主要潜力是作为混合动力油(致密油和页岩油)。中国页岩在时间和空间上是非均质的,高质量的页岩储层通常位于海侵系统地带至早高架系统地带区间内,这些区间以缺氧沉积环境沉积。对于中国的页岩气而言,构造运动影响并破坏了早期的油气聚集,从而使构造稳定的地区成为页岩气勘探和开发的更有利前景。

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