首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Left-lateral sense offset of Upper Proterozoic to Paleozoic features across the Gobi Onon, Tost, and Zuunbayan faults in southern Mongolia and implications for other central Asian faults
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Left-lateral sense offset of Upper Proterozoic to Paleozoic features across the Gobi Onon, Tost, and Zuunbayan faults in southern Mongolia and implications for other central Asian faults

机译:蒙古南部戈壁Onon,Tost和Zuunbayan断层上元古界到古生界特征的左向偏移及其对其他中亚断层的影响

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摘要

We present a preliminary study of Upper Proterozoic to Paleozoic features adjacent to, and offset across, three faults in southern Mongolia. Restoration of four offset stratigraphic units adjacent to the Gobi Onon fault indicates a left-lateral sense offset of 70-95 km. The Tost fault has a left-lateral sense offset of 95-125 km defined by three offset features. The Zuunbayan fault has seven offset features that display left-lateral sense offsets of 185-235 km. Deformation on these faults apparently occurred during the Mesozoic prior to the Late Cretaceous based upon the age of offset features, the age of overlap sequences, and inferred timing relationships with regional contractional structures. Although Cenozoic overprinting and reactivation has occurred along parts of these faults, thus complicating their restorations, we present a testable hypothesis which predicts possible connections between these faults and faults within China.
机译:我们对与蒙古南部三个断层相邻并错开的上元古代至古生代特征进行了初步研究。与戈壁Onon断层相邻的四个偏移地层单位的恢复表明左方向感测偏移为70-95 km。 Tost断层的左向偏移量为95-125 km,由三个偏移量特征定义。 Zuunbayan断层具有七个偏移特征,显示的左侧偏移为185-235 km。这些断层的变形显然是在白垩纪晚期的中生代之前发生的,这是基于偏移特征的年龄,重叠层序的年龄以及推断的与区域收缩结构的时间关系。尽管沿这些断层的某些部分发生了新生代叠印和活化作用,使它们的修复复杂化,但我们提出了可检验的假设,该假说预测了这些断层与中国内部断层之间的可能联系。

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