春雅河流域(西伯利亚地台通古斯河podkamennaya右支流)上奥陶统生物地层学

Q4 Earth and Planetary Sciences
T. Gonta, A. Timokhin, O. Maslova
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引用次数: 0

摘要

本文介绍了西伯利亚地台楚亚河流域(通古斯河波德卡门纳河右支流)上奥陶统曼加济亚组剖面的研究成果。所给出的逐层剖面描述和主要动物群(介形虫、三叶虫、腕足类、牙形刺)的新数据,使包围沉积物的古生物学特征得到了显著扩展。Baksan层位沉积的描述是首次给出的,它更新了先前对Upper Chunku R.河口上方2公里处Dolbor层位的层型剖面下底地层的描述。根据已发表的资料和新获得的数据,对不同的动物群进行了生物地层分析,从而有可能澄清位于阿穆特干河口以下0.4公里处的剖面的地层位置。将研究剖面与Gaindinskaya-3试井进行了对比。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
THE UPPER ORDOVICIAN BIOSTRATIGRAPHY OF THE CHUNYA RIVER BASIN (RIGHT TRIBUTARY OF THE PODKAMENNAYA TUNGUSKA RIVER, SIBERIAN PLATFORM)
The article deals with presented results of studying Upper Ordovician sections of the Mangazeya Formation in the Chuya River basin (right tributary of the Podkamennaya Tunguska River) of the Siberian Platform. The given layer by layer section description and new data on leading groups of fauna (ostracods, trilobites, brachiopods, conodonts) allowed for significantly expanding paleontological characteristics of enclosing sediments. The description of the Baksan Horizon deposits is given for the first time, it updates the earlier description of underlying formations in the stratotypic section of the Dolbor Horizon 2 km above the mouth of the Upper Chunku R. (left bank). As a result of biostratigraphic analysis for different groups of fauna, both from published sources and newly obtained data, it has become possible to clarify the stratigraphic position of the section located 0.4 km below the mouth of the Amutkan River. The correlation of studied sections with the Gaindinskaya-3 test well was carried out.
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来源期刊
Geology and Mineral Resources of Siberia
Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology
CiteScore
0.30
自引率
0.00%
发文量
23
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