基于古地磁资料的苏甘斯克沉积盆地古地理(奥列内克隆起带温甸)

Trofimuk Readings - 2021: Proceedings of the All-Russian Youth Scientific Conference with the Participation of Foreign Scientists Pub Date : 1900-01-01 DOI:10.25205/978-5-4437-1251-2-33-37

K. A. Pakhomova, D. Drozdov

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引用次数: 0

摘要

本文根据古地磁记录，重建了西伯利亚地台苏甘斯克沉积盆地5.6 ~ 5.5亿年前的古地理位置。khatyspt组是一个很有希望的研究对象，因为该组的文代年龄是有效的，岩石几乎没有变形，也没有发生化学变化。根据磁化成分的研究结果，在Khatyspyt组成藏时苏甘斯克沉积盆地的位置与南纬38.8°相匹配。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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PALEOGEOGRAPHY OF THE SUKHANSK SEDIMENTARY BASIN BASED ON PALEOMAGNETIC DATA OF KHATYSPYT FORMATION (VENDIAN OF OLENEK UPLIFT)

The present work is about reconstruction of the paleogeographic position of the Sukhansk sedimentary basin of the Siberian platform for a time interval of 560–550 million years ago on the basis of a paleomagnetic record. A promising object for this researche is the Khatyspyt Formation, because Vendian age of this formation is valid, the rocks are practically not deformed and did not undergo chemical changes. The position of the Sukhansk sedimentary basin at the time of the accumulation of the Khatyspyt Formation match to 38,8° southern latitude according to the results of studying the component composition of magnetization.

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Trofimuk Readings - 2021: Proceedings of the All-Russian Youth Scientific Conference with the Participation of Foreign Scientists

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