基于构造物理模拟实验的桌子山煤田棋盘井井田奥灰边界构造因素分析Ordovician Limestone Boundary Structural Factor Analysisin Qipanjing Minefield, Zhuozishan Coalfield Based on Tectonic Physical Simulation Experiment
张国俊,黄金荣,鲁欣,王占军,史志江
摘要(Abstract):
棋盘井井田位于桌子山煤田东南缘,以苛素乌断层为界分为东西两区,东区奥灰缺失,成因机理尚不明确。在分析研究区地质构造格架、井田地质构造的基础上,结合构造物理模拟实验,研究了构造作用对奥灰地层缺失的影响。结果表明:桌子山地区构造几何形态和构造物理模拟结果高度相似,反映出棋盘井井田苛素乌边界断裂可能是顺基底的滑脱作用造成的,且改变了奥陶系灰岩沉积的原始边界,使得沉积边界向东迁移。
关键词(KeyWords): 奥陶系;地层缺失;砂箱物理模拟实验;棋盘井井田
基金项目(Foundation): 国家自然科学基金项目“龙门山构造带南段中-新生代构造变形研究”(41602212);; 中国博士后科学基金面上项目“龙门山南段前陆构造扩展带构造变形特征与变形过程研究”(2019M653694)
作者(Author): 张国俊,黄金荣,鲁欣,王占军,史志江
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