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机构地区:[1]中国石油大学北京油气资源与探测国家重点实验室,北京102249
出 处:《西北大学学报(自然科学版)》2009年第3期392-398,共7页Journal of Northwest University(Natural Science Edition)
基 金:国家自然科学基金资助项目(40872143);油气资源与探测国家重点实验室开放基金资助项目(PRPZY2008-01)
摘 要:目的系统研究韧性基底层黏度对褶皱-冲断带变形特征的影响。方法采用不同韧性基底层黏度砂箱模型进行系列实验。结果韧性基底层在黏度较高的情况下,褶皱-冲断带以前冲断层为主导,并以前展方式扩展。随着韧性基底层黏度的降低,后冲断层逐渐占主导,形成双冲向、且比较典型的隔槽式褶皱-冲断带。结论韧性基底层黏度对褶皱-冲断带变形演化具有十分显著的影响,宽阔低锥度的双冲向褶皱-冲断带的形成可能与其下伏存在的软弱基底层有关。韧性基底层的存在是形成隔槽式褶皱-冲断构造样式的重要因素。Aim To systematically investigate the influence of viscosity of ductile substrate on deformational features of fold-and-thrust belts. Methods Experiments of a series of sandbox models with a ductile substrate of different viscosities were conducted. Results The experimental results show that fold-and-thrust belts formed in the models with substrata of high viscosity are predominated by forward-vergent thrusts and develop in a frontward sequence. As the viscosity of substrata deereases, rearward-vergent thrusts gradually increase and fold-and-thrust belts are often predominated by dual vergent thrusts and consist of typical trough-like folds. Conclusion It is indicated that viscosity of substrata has played an important role in deforation evolution of fold-and-thrust belts. Wider fold-and-thrust belts of lower taper and dual vergenee are probably related to their weak substrata. Existence of ductile substrate is an important factor in the formation of trough-like folds in a fold-and-thrust belt.
分 类 号:P544.43[天文地球—构造地质学]
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