扬子地块西南缘瓮安穹隆不整合面特征、年代限定及大地构造意义
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摘要
瓮安穹隆位于近南北向的鄂渝湘黔穹隆群构造带与东西向黔中隆起的过渡区域,本质上为一构造叠加穹隆。瓮安穹隆及周缘发育并完好地保留了加里东期、印支期和燕山期不整合面。这些对应于关键构造事件的不整合面的发育特征和年代限定是进行区域和大地构造重建的重要手段。研究结果表明:(1)古生代以来瓮安穹隆及邻区构造格局出现3次重大变动,先后经历了加里东期、印支期、燕山期等3个关键演化阶段,是前震旦陆壳基底上的叠加穹隆。早古生代以来,瓮安穹隆及邻区主要发育中志留统顶面(S_2/AnS_2)、中三叠统顶面(T_2/AnT_2)、中侏罗统顶面(J_2/AnJ_2)不整合,分别与加里东期、印支期和燕山期构造运动有关。(2)根据碎屑锆石年龄分布统计结果,瓮安地区及邻区加里东运动的发生时间为426～415 Ma,印支运动的发生时间为246～233Ma,燕山运动发生的时间为168～150 Ma。对瓮安穹隆出现的不整合进行构造及年代学分析,从而进一步探讨穹隆的构造演化,将有助于对穹隆构造的深入研究。
The Weng'an Dome is located in the transitional region between the Hubei-Chongqing-HunanGuizhou dome group in near N-S direction and the Qianzhong Uplift in the E-W direction.Our research suggests that the Weng'an Dome is essentially a superimposed tectonic dome.Caledonian,Indosinian and Yanshanian unconformities are developed and well retained in the Weng'an Dome and its surrounding area.Unconformity characteristics corresponding to key tectonic events and age constraint are important factors in reconstructing regional geology and tectonics.Our results can be summarized as follows:(1)The Weng'an Dome experienced three major deformations during the Paleozoic and Mesozoic.It is a superimposed tectonic dome with cratonic basement.The S_2/AnS_2,T_2/AnT_2 and J_2/AnJ_2 unconformities are distinguishable within the Weng'an Dome and its surrounding area,and they correspond to the Caledonian,Indosinian and Yanshanian tectonic movements in the Yangtze Block,respectively.And(2)The ages of unconformities,constrained by using detrital zircon U-Pb method,demonstrate that the Caledonian,Indosinian and Yanshanian tectonic events occurred during 426-415,246-233 and 168-150 Ma,respectively.Through structural and chronological analyses of unconformities,we also explored the tectonic evolution of the dome,which shall contribute to the in-depth study of the dome structure.
The Weng'an Dome is located in the transitional region between the Hubei-Chongqing-HunanGuizhou dome group in near N-S direction and the Qianzhong Uplift in the E-W direction.Our research suggests that the Weng'an Dome is essentially a superimposed tectonic dome.Caledonian,Indosinian and Yanshanian unconformities are developed and well retained in the Weng'an Dome and its surrounding area.Unconformity characteristics corresponding to key tectonic events and age constraint are important factors in reconstructing regional geology and tectonics.Our results can be summarized as follows:(1)The Weng'an Dome experienced three major deformations during the Paleozoic and Mesozoic.It is a superimposed tectonic dome with cratonic basement.The S_2/AnS_2,T_2/AnT_2 and J_2/AnJ_2 unconformities are distinguishable within the Weng'an Dome and its surrounding area,and they correspond to the Caledonian,Indosinian and Yanshanian tectonic movements in the Yangtze Block,respectively.And(2)The ages of unconformities,constrained by using detrital zircon U-Pb method,demonstrate that the Caledonian,Indosinian and Yanshanian tectonic events occurred during 426-415,246-233 and 168-150 Ma,respectively.Through structural and chronological analyses of unconformities,we also explored the tectonic evolution of the dome,which shall contribute to the in-depth study of the dome structure.
引文
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