首页> 外文期刊>Russian journal of Pacific geology >Provenance of the Middle Jurassic-Lower Cretaceous (Berriasian-Valanginian) deposits of the Lower Amur region
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Provenance of the Middle Jurassic-Lower Cretaceous (Berriasian-Valanginian) deposits of the Lower Amur region

机译:下阿穆尔河地区中侏罗统-下白垩统(贝里亚斯-瓦朗吉尼亚)矿床的物源

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摘要

The petrographic and chemical study of the Middle Jurassic-Lower Cretaceous rocks of the Lower Amur region revealed the important role of granitoids in their provenance. Intermediate, mafic, and ultramafic (?) intrusive rocks, as well as sedimentary, volcanic, and metamorphic complexes were less common. The orientation of the cross bedding and casts of whirlpool pits in the Tithonian-Valanginian turbidites indicates that the provenance was located in the west and southwest. It was mainly made up of the continental granite-metamorphic blocks of the Jiamusi-Khanka-Bureya Massif. At the same time, a significant part of the provenance was occupied by the fragments of the Late Paleozoic-Early Mesozoic active continental margin.
机译:对下阿穆尔河地区中侏罗世-下白垩纪岩石的岩石学和化学研究表明,类花岗岩在其物源中具有重要作用。中,镁铁质和超镁铁质(?)侵入岩,以及沉积,火山和变质复合体较少见。 Tithonian-Valanginian浊积岩中的交叉地层和漩涡坑铸件的方向表明,物源位于西部和西南部。它主要由佳木斯-汉卡-布雷亚地块的花岗岩花岗岩变质块组成。同时,大量的物源被晚古生代-早中生代活动大陆边缘的碎片所占据。

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