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U-Pb Age of Detrital Zircons from the Upper Precambrian Terrigenous Section of North Timan

机译:北提曼上前寒武纪陆生陆段碎屑锆石的U-Pb年龄

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摘要

In terms of neotectonics, the Timan Range and Kanin Peninsula represent a spacious mountainous structure 1150 km long and 80-160 km wide extending in the northwesterly direction from Mount Poly-udov Kamen to Cape Kanin Nos in the Kanin Peninsula. It consists of isolated en echelon arranged horst-like uplifts with Upper Precambrian rocks cropping out in their arch parts. In the southwest the Timan Range borders the Pechora Plate that frames the Karelian part of the East European Platform in the northeast. The boundary between the Pechora Plate and Mezen megablock of the East European Platform corresponds to the West Timan deep-seated fault.
机译:就新构造而言,提曼山脉和卡宁半岛代表着一个宽阔的山区结构,长1150公里,宽80-160公里,向西北方向延伸,从波多乌多夫卡门山到卡宁半岛的卡宁角。它由孤立的梯队组成的霍斯特状隆起组成,上拱前部分钻出上寒武统岩石。在西南部,提曼山脉(Timan Range)与Pechora板块接壤,后者构成了东北部东欧平台的卡累利阿山脉部分。东欧平台的Pechora板块和Mezen巨块之间的边界对应于West Timan深部断层。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|592-596|共5页
  • 作者单位

    Institute of Geology, Komi Scientific Center, Ural Branch, Russian Academy of Science, Pervomaiskaya 54, Syktyvkar, 167982 Russia;

    Institute of Geology, Komi Scientific Center, Ural Branch, Russian Academy of Science, Pervomaiskaya 54, Syktyvkar, 167982 Russia;

    Department of Geosciences, University of Arizona, Tucson, Arizona, 85721 USA;

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