首页> 外文期刊>Russian journal of Pacific geology >New finds of middle and late jurassic radiolarians in the siliceous-clayey and clastic rocks of the Nadan'khada-Bikin terrane (Jurassic accretionary wedge, western Sikhote Alin) and their geological significance
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New finds of middle and late jurassic radiolarians in the siliceous-clayey and clastic rocks of the Nadan'khada-Bikin terrane (Jurassic accretionary wedge, western Sikhote Alin) and their geological significance

机译:在Nadan'khada-Bikin地层的硅质黏土和碎屑岩中(侏罗纪增生楔形物,西锡克特阿林西部)新发现的中晚侏罗世放射虫及其地质意义

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摘要

The lithostratigraphic analysis of the paleo-oceanic sediments in the Bikin segment of the Nadan'khada-Bikin terrane of the Jurassic accretionary wedge revealed late Bajocian and early to middle Bathonian radiolarians in the siliceous-clayey rocks constituting its southern part in the Perepelinaya-Cheremshanka and Kedrovka areas. Siltstones from the central part of the Bikin segment in the upper reaches of the Vasil'eka River contain radiolarians of the terminal late Tithonian age. Combined with the known dates available for siliceous-clayey rocks from the western part of the Nadan'khada Alin Range and the Ulitka-Zolotoi Klyuch area, these data made it possible to define three stages in the formation of the Bikin segment of the Nadan'khada-Bikin terrane of the accretionary wedge: the terminal Middle Jurassic, the late Tithonian, and the Berriasian. The formation of this segment lasted approximately 25 Ma.
机译:侏罗纪增生楔Nadan'khada-Bikin地层Bikin段古海洋沉积的岩体地层学分析显示,在Perepelinaya-Cheremshanka南部的硅质-粘土岩石中,巴乔期晚期和中巴东期放射弧成岩。和科德罗夫卡地区。瓦西里卡河上游的比金河段中部的粉砂岩含有蒂通期末期的放射虫。结合来自Nadan'khada Alin山脉西部和Ulitka-Zolotoi Klyuch地区的硅质粘土岩石的已知日期,这些数据使得可以确定Nadan'Bikin段形成的三个阶段。增生楔的khada-Bikin地层:中侏罗世末期,铁通晚期和贝里亚斯期。该段的形成持续了大约25 Ma。

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