波卢斯尼地层中心区(北雅库特)中-上侏罗世沉积物的年龄和成分

IF 0.7 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
E. V. Vatrushkina, M. V. Gertseva, V. V. Kostyleva, S. D. Sokolov
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引用次数: 0

摘要

摘要 介绍了关于波卢斯尼地层中央区侏罗纪地段的组成和结构的新数据。岩相学数据确定了砂岩的岩石成分和沉积物来源中花岗岩的主要成分。在砂岩中发现了各种成分的火山岩再沉积碎片和同步火成碎屑物质。通过对碎屑锆石的铀-铅同位素年代测定以及所获得的最大沉积年龄,可以对中央区出露的侏罗纪沉积物的地层体积进行修正,并将其限定为上巴约卡期至提托尼期。成分的不成熟和没有可靠年代的赫坦纪-阿伦纪沉积物表明了一个新的沉积周期,并与三叠纪-侏罗纪存在单一的上霍扬斯克被动边缘相矛盾。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Age and Composition of the Middle–Upper Jurassic Sediments in the Central Zone of the Polousnyi Terrane (Northern Yakutia)

Age and Composition of the Middle–Upper Jurassic Sediments in the Central Zone of the Polousnyi Terrane (Northern Yakutia)

Abstract

New data on the composition and structure of the Jurassic section in the Central zone of the Polousnyi Terrane are presented. The arkosic composition of sandstones and the predominance of granites in the sediment provenance was established by petrographic data. Both redeposited fragments of volcanic rocks of various composition and synchronous pyroclastic material were identified in the sandstones. U–Pb isotope dating of detrital zircons and the obtained maximum depositional age made it possible to revise the stratigraphic volume of the Jurassic sediments exposed in the Central Zone and to limit it from the Upper Bajocian to the Tithonian. The immaturity of the composition and the absence of reliably dated Hettangian–Aalenian sediments indicate a new cycle of sedimentation and contradict the existence of a single Verkhoyansk passive margin in the Triassic–Jurassic.

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来源期刊
Doklady Earth Sciences
Doklady Earth Sciences 地学-地球科学综合
CiteScore
1.40
自引率
22.20%
发文量
138
审稿时长
3-6 weeks
期刊介绍: Doklady Earth Sciences is a journal that publishes new research in Earth science of great significance. Initially the journal was a forum of the Russian Academy of Science and published only best contributions from Russia. Now the journal welcomes submissions from any country in the English or Russian language. Every manuscript must be recommended by Russian or foreign members of the Russian Academy of Sciences.
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