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Controlling effect of texture on fracability in lacustrine fine-grained sedimentary rocks

机译:纹理对湖泊细粒沉积岩下可脱水性的控制效果

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摘要

Microtextures in lacustrine fine-grained sedimentary rocks generally include the basic features of quantity, size, shape and arrangement of particles, which are the internal factors that affect the mechanical properties of rocks. In this paper, based on mechanical experiments and a rock slice image analysis technique, fracability is systematically evaluated in terms of textures by using the Mesozoic and Cenozoic lacustrine fine-grained sedimentary rocks in eastern China. Analysis show that the fracability of fine-grained sedimentary rocks is improved with increasing particle quantity and size but is reduced with increasing particle sorting, roundness, vertical distribution uniformity and holistic distribution uniformity. Regarding composition, fracability is reduced with increases in clay minerals and total organic carbon (TOC) but is first reduced and then improved with increases in the content of feldspar or carbonate minerals, i.e., when the mineral content exceeds 30%, fracability is positively correlated with it, but it is negatively or weakly correlated for mineral contents below 30%. Fracability is improved with enhanced the diagenesis strength. Regarding structural aspect, the fine-grained sedimentary rocks with strong laminability and continuity have poor fracability. A comparative analysis also shows that the stronger control factors on fracability are vitrinite reflectance (Ro), particle quantity, size, sorting, roundness and holistic distribution uniformity, while the components (e.g., TOC, clay minerals, and felsic minerals) and laminar development degree (e.g., laminar continuity and laminar quantity) are relatively weak factors. Diagenesis plays an important role in fracability for the fine-grained sedimentary rocks in different target layers, but for the fine-grained sedimentary rocks in a target layer, the texture factors are the intrinsic factors controlling the fracability and should be considered as primary considerations in engineering fracturing operations.
机译:Lapustrine细粒细粒沉积岩中的微型纹理通常包括颗粒的数量,尺寸,形状和布置的基本特征,这是影响岩石力学性能的内部因素。本文在机械实验和岩石切片图像分析技术的基础上,通过使用东部地区的中生代和新生代宽容细粒细粒细粒沉积物来系统地评估可脱离可变性。分析表明,随着粒子量和尺寸的增加,细粒沉积岩的可脱水性得到改善,但随着颗粒分选,圆度,垂直分布均匀性和整体分布均匀性而降低。关于组合物,随着粘土矿物质和总有机碳(TOC)的增加,减少脱离可脱离性,但是首先减少,然后随着长石或碳酸盐矿物质的含量的增加而改善,即,当矿物质含量超过30%时,可脱水性正相关用它,但对于低于30%的矿物质含量是负面的或弱弱。随着成岩作用强度提高,可脱离可脱水性。关于结构方面,具有强大的薄层和连续性的细粒沉积岩具有差的可脱落性。比较分析还表明,对脱水性的更强的控制因素是vitriinite反射率(RO),粒子量,尺寸,分选,圆度和整体分布均匀性,而组件(例如,TOC,粘土矿物质和纤维矿物)和层流发育程度(例如,层流连续性和层流量)是相对较弱的因素。成岩作用在不同靶层中的细粒沉积岩石中的可脱离可变作用起着重要作用,但对于靶层中的细粒沉积岩,纹理因素是控制脱离症的内在因素,并且应该被视为主要考虑因素工程压裂操作。

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