首页> 外文期刊>Science in China. Series D, Earth sciences >Experimental remolding on the caprock's 3D strain field of the Indosinian-Yanshanian epoch in Tongling deposit concentrating area
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Experimental remolding on the caprock's 3D strain field of the Indosinian-Yanshanian epoch in Tongling deposit concentrating area

机译:铜陵矿床集中区印支期-燕山期的盖层3D应变场实验重塑

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摘要

Based on field observations and rheology analysis, we perform one analogue experiment and remold the 3D structural frame of Tongling deposit concentrating area firstly. Then we disassemble and dialyze the 3D structures of the model using the methods of "slicing" and "stripping". A series of sliced planes vertical to the fold hinges show similar landscapes of that in the drill hole profiles. Meanwhile, layer stripping analysis indicates that the deformation features of each layer in the model are qualitatively analogical to those obtained from field observations. Through contrasting the 3D structure between the experimental model and the field phenomena, we verify the following 3D deformation features of the caprock in this area: (1) the Tongling area mainly consists of three series of NE S-typed fold groups; (2) in the uniform stress field, the incoherent folds universally develop in different positions, along different axes as well as in different strata; (3) the faults propagate upward which are mostly inter-bedded detachment faults, while the fold amplitudes decrease while going deeper; and (4) the folds and cleavages are highly developed in the Silurian System indicating that the deformation effect of the Indosinian-Yanshanian structural layer terminates at this layer, which suggests that the Silurian System is the crucial layer for the inversion between brittle and plastic deformation domains and the underlying strata are subject to the control of another deformation system with distinct properties.
机译:在现场观察和流变学分析的基础上,我们进行了一次模拟实验,首先对铜陵矿床集中区的3D结构框架进行了改造。然后,我们使用“切片”和“剥离”方法拆卸并透析模型的3D结构。垂直于折页铰链的一系列切片平面在钻孔轮廓中显示出相似的风景。同时,层剥离分析表明,模型中每一层的变形特征在质量上与实地观测的相似。通过对比实验模型和野外现象之间的3D结构,我们验证了该区域盖层的以下3D变形特征:(1)铜陵地区主要由3个NE S型褶皱群组成。 (2)在均匀应力场中,不连贯褶皱普遍分布在不同的位置,沿不同的轴线以及不同的地层。 (3)断层向上传播,多为层间分离断层,向深层褶皱幅度减小。 (4)志留纪系统中褶皱和裂理高度发育,表明印支期-燕山期构造层的变形作用终止于这一层,这表明志留纪系统是脆性和塑性变形反演的关键层。区域和下伏地层都受具有不同属性的另一个变形系统的控制。

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