中提曼岛叠层石的新位置:其形态和结构特征

E. Antropova
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引用次数: 0

摘要

本文介绍了对沃雷克瓦河左岸(中提曼河)一个新地点的帕维尤加地层中的里普安期叠层石进行宏观和微观研究的结果。这些叠层石形成了一个叠层石生物圈。叠层石群的微观结构具有不同成分和粒度的分层特征;在微粒状夹层中发现了凝块型和丝状型有机形成的痕迹。还发现了许多二次转化的痕迹,如黄铁矿化、贝壳白云石化和栅栏形成。叠层石在分类学上属于 Gimnosolen sp.和 Inseria djejimi Raab.在帕维尤加地层的上部也发现了类似的组合,但该组合中的叠层石群排列紊乱,这表明了有机质堆积边缘的环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A new location of stromatolites in the Middle Timan: their morphological and structural features
The paper presents the results of macroscopic and microscopic study of Riphean stromatolites of the Pavyuga Formation from a new locality on the left bank of the Vorykva River (Middle Timan). The stromatolites form a stromatolite bioherm. The microstructure of the stromatolite assemblages is characterised by layering of different composition and granularity; traces of organogenic formations of clotted and filamentous type were found in microgranular interlayers. Numerous traces of secondary transformations, such as pyritization, dolomitization on shells, and fenestra formation, were noted. The taxonomic affiliation of the stromatolites to the species Gimnosolen sp. and Inseria djejimi Raab. allows dating to the Late Riphean. A similar association is known from the upper part of the Pavyuga Formation, but the colonies of stromatolites are orientated disorderly in that association, which indicates the environment of the organogenic buildup margins.
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