First Data on Late Cretaceous Terrigenous Deposits of the Upper Part of the Zhuravlevka–Amur Terrane Section in the Lower Amur River Area: Evidence from U/Pb Detrital Zircon Geochronology

IF 0.9 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
I. A. Alexandrov, A. I. Malinovsky, V. V. Ivin, S. Yu. Budnitskiy
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引用次数: 0

Abstract

The paper reports data on the age and composition of poorly studied Cretaceous clastic rocks of the Lower Amur River area, which are part of the Zhuravlevka–Amur terrane and are attributed to the Berriasian–Valanginian Komsomolsk series. U/Pb dating of detrital zircons yielded reliable dates of 99 and 90 Ma for the Gorin and Pioneer formations, respectively. Thus, a sedimentary complex with a Late Cretaceous sedimentation age was identified for the first time in the Sikhote-Alin orogenic belt based on detrital zircon geochronology. In composition and detrital zircon age distribution pattern, the studied rocks are more similar to sediments of the upper, Hauterivian–Albian part of the Zhuravlevka–Amur terrane section rather than to those of the lower, Berriasian–Valanginian part. In rocks of the Pioneer Formation, the youngest zircon population with an age of about 90 Ma makes up more than 40% of all dated grains. The main source of detrital material of this age was probably proximal andesites hosting the Mnogovershinnoe deposit and granitoids of the Nizhneamurskii Complex. The source of detritus for sediments of the ∼99 Ma Gorin Formation was probably felsic rocks from the Albian–Cenomanian igneous province of Pacific Asia. The discrepancy between the Late Cretaceous age obtained by us and the paleontologically established Berriasian–Valanginian stratigraphic age of the formations requires additional research. New data on the Late Cretaceous age of the Zhuravlevka–Amur sediments of strike-slip marginal-continental basin requires revision of the geologic evolution of the terrane and the entire Sikhote-Alin orogenic belt.

Abstract Image

阿穆尔河下游地区朱拉夫列夫卡-阿穆尔地层段上部晚白垩世土著沉积的第一批数据:U/Pb锆英石地质学证据
本文报告了对阿穆尔河下游地区白垩纪碎屑岩的年龄和组成研究较少的数据,这些碎屑岩是Zhuravlevka-阿穆尔地层的一部分,属于白垩纪-瓦朗基尼共青城系。对碎屑锆石进行的 U/Pb 测定结果表明,戈林地层和先锋地层的可靠年代分别为 99 和 90 Ma。因此,根据碎屑锆石地质年代学,首次在锡霍特-阿林造山带发现了具有晚白垩世沉积时代的沉积复合体。在成分和锆英石年龄分布模式上,所研究的岩石更类似于朱拉夫列夫卡-阿穆尔地层段上部豪特里维-阿尔卑斯时期的沉积物,而不是下部白垩纪-瓦朗金时期的沉积物。在先锋地层的岩石中,年龄约为 90 Ma 的最年轻锆石群占所有已测定年代的锆石颗粒的 40% 以上。这一年龄段的碎屑物质的主要来源可能是Mnogovershinnoe矿床的近安山岩和Nizhneamurskii复合体的花岗岩。99 Ma ∼ 99 Ma 戈林地层沉积物的碎屑来源可能是太平洋亚洲阿尔卑斯-仙人掌火成岩带的长英岩。我们获得的白垩纪晚期年龄与古生物学确定的白垩纪-瓦朗基年地层年龄之间的差异需要进一步研究。关于走向滑动边缘大陆盆地茹拉夫列夫卡-阿穆尔沉积物晚白垩世年龄的新数据要求对该地层和整个锡霍特-阿林造山带的地质演化进行修订。
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来源期刊
Russian Journal of Pacific Geology
Russian Journal of Pacific Geology 地学-地球科学综合
CiteScore
1.30
自引率
37.50%
发文量
34
审稿时长
>12 weeks
期刊介绍: Russian Journal of Pacific Geology publishes the results of research on the Earth crust and mantle composition and provides articles on the geological structure and patterns of distribution of mineral deposits in the Pacific Ocean, marginal seas and continental margins. It discusses the topics of stratigraphy, sedimentology, magmatic activity, and seismicity. The journal deals with the problems of lithosphere plates tectonics, and offers the results of neotectonic, geomorphological, geodesic, environmental and mining studies in the Pacific region. The journal accepts theoretical, methodical and philosophical articles covering general issues of geology, geophysics, geochemistry, geoecology and mining. The journal also publishes critical notes and comments, and reviews.
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