萨拉托夫右岸南部古新世侦察磁地层研究结果

D. A. Shelepov, A. Guzhikov
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摘要

本文介绍了萨拉托夫右岸下Syzran亚组(古新世)两个剖面——Syrt山(Nizhnyaya Bannovka村)和Lysaya Gora(萨拉托夫市)的岩石磁和古地磁研究结果。首次建立了在岩石部分再磁化的情况下获得伏尔加地区古新世古地磁资料并用于磁地层学研究的可能性。展望了利用矿床岩石磁性特征进行剖面详细对比和沉积学重建的前景。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Results of the reconnaissance magnetostratigraphic studies of Paleocene in the southern part of the Saratov right bank
The results of rock-magnetic and paleomagnetic studies of two sections of the Lower Syzran subformation (Paleocene) of the Saratov Right Bank – the Syrt Mountain (Nizhnyaya Bannovka village) and Lysaya Gora (Saratov city) are presented. For the first time the possibility of obtaining paleomagnetic data on the Paleocene of the Volga region and their use for magnetostratigraphic purposes despite the partial remagnetization of rocks has been established. The prospects of using rock-magnetic characteristics of deposits for detailed correlations of sections and sedimentological reconstructions are demonstrated.
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