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Well log evaluation of shale gas reservoirs and preservation conditions of Lower Cambrian shale succession in Cengong Block of southeast Sichuan basin, south China

机译:四川盆地东南部岑巩区块页岩气储层测井评价及下寒武统页岩演替保存条件

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The abundant lower Cambrian marine shale gas resources discovered in south China is of great potential for exploitation. In particular, Cengong Block, which is located in a complex tectonic deformation region of southeast Sichuan basin, south China, is one of the marine shale gas exploring areas currently. In this area, folds and faults are well developed, mainly strike in NE or NNE directions. Lower Cambrian marine shale is characterized by great thickness and regional extensive distribution. Lower Cambrian strata in this region is mainly consisted of deep shelf deposits. Sandstone and limestone are determined based on GR log and neutron-density cross plot. Lower Cambrian shales in Cengong Block are associated with high GR value and TOC. Relatively low content of Thorium (Th) and Potassium (K) indicates low clay content. Neutron-density crossover is usually associated with gas-bearing shale beds. Brittle shale beds are well developed and the gas storage capacity of lower Cambrian shale reservoir has been affected by faulting and folding to some extent. Small-scale water-bearing caves are developed in the limestones and dolomites of lower Cambrian strata which usually displays low-pressure anomalies. Although the lower Cambrian shale reservoir in study area is characterized with distinct gas-bearing properties and shale gas flow has been obtained after fracturing, it is essential to recognize that the preservation conditions of shale gas accumulation are affected by tectonics, formation water and pressure coefficient. (C) 2016 Elsevier B.V. All rights reserved.
机译:在中国南部发现的丰富的下寒武统海相页岩气资源具有巨大的开采潜力。特别是位于中国东南部四川盆地东南部复杂构造变形区的岑巩区块,是目前海相页岩气勘探区之一。在该地区,褶皱和断层发育良好,主要发生在东北或北非方向。下寒武统海相页岩的特点是厚度大,区域分布广泛。该地区的下寒武统地层主要由深架沉积物组成。根据GR log和中子密度交叉图确定砂岩和石灰岩。岑贡区块下寒武统页岩与高GR值和TOC有关。 Thor(Th)和钾(K)含量相对较低,表明粘土含量较低。中子密度交换通常与含气页岩床有关。脆性页岩床发育良好,下寒武统页岩储层的储气能力在一定程度上受到断层和褶皱的影响。下寒武统地层的石灰岩和白云岩中发育了小规模的含水洞穴,这些洞穴通常表现出低压异常。尽管研究区下寒武统页岩储层具有明显的含气性,压裂后获得了页岩气流动,但必须认识到页岩气聚集的保存条件受构造,地层水和压力系数的影响。 。 (C)2016 Elsevier B.V.保留所有权利。

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