The Lithological and Geochemical Features and Paleoclimatic Conditions for the Formation of the Verkhnyaya Lena Group (Southeast of the Siberian Platform)

IF 0.3 Q4 GEOLOGY Moscow University Geology Bulletin Pub Date : 2024-02-07 DOI:10.3103/s0145875223050095
S. I. Merenkova, I. V. Korovnikov, R. R. Gabdullin
{"title":"The Lithological and Geochemical Features and Paleoclimatic Conditions for the Formation of the Verkhnyaya Lena Group (Southeast of the Siberian Platform)","authors":"S. I. Merenkova, I. V. Korovnikov, R. R. Gabdullin","doi":"10.3103/s0145875223050095","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>The Verkhnyaya Lena Group (Є<sub>2–3</sub><i>vl</i>) has been studied in a section on the right bank of the Malaya Chuya River. Concentrations of main oxides and some trace elements (Cr, V, Ni, Cu, Zn, Rb, Sr, Zr, Ba, U, Th, Y, Nb, and Cl) have been determined in samples using an X-ray spectral fluorescence (XRF) analysis. The normative mineral composition has been determined based on the results of the XRF analysis using the MINLITH software. Based on geochemical data, intervals of change in the weathering features (physical/chemical and arid/humid weathering) are clearly differentiated in the denudation area, which are fixed by variations in the values of the Al<sub>2</sub>O<sub>3</sub>/K<sub>2</sub>O and Ln(Al<sub>2</sub>O<sub>3</sub>/Na<sub>2</sub>O) ratios and concentrations of V, Cu, Zn, Rb, and Ni, as well as the normative mineral composition. Apparently, Cr was transported to the basin exclusively by the aeolian process in this case and marks periods of increased wind transport intensity. Under conditions of tectonic activation and progressive isolation of the Upper Lena paleobasin, the described lithological and geochemical features provide some information about the climate changes that accompanied these events.</p>","PeriodicalId":44391,"journal":{"name":"Moscow University Geology Bulletin","volume":null,"pages":null},"PeriodicalIF":0.3000,"publicationDate":"2024-02-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Moscow University Geology Bulletin","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3103/s0145875223050095","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

The Verkhnyaya Lena Group (Є2–3vl) has been studied in a section on the right bank of the Malaya Chuya River. Concentrations of main oxides and some trace elements (Cr, V, Ni, Cu, Zn, Rb, Sr, Zr, Ba, U, Th, Y, Nb, and Cl) have been determined in samples using an X-ray spectral fluorescence (XRF) analysis. The normative mineral composition has been determined based on the results of the XRF analysis using the MINLITH software. Based on geochemical data, intervals of change in the weathering features (physical/chemical and arid/humid weathering) are clearly differentiated in the denudation area, which are fixed by variations in the values of the Al2O3/K2O and Ln(Al2O3/Na2O) ratios and concentrations of V, Cu, Zn, Rb, and Ni, as well as the normative mineral composition. Apparently, Cr was transported to the basin exclusively by the aeolian process in this case and marks periods of increased wind transport intensity. Under conditions of tectonic activation and progressive isolation of the Upper Lena paleobasin, the described lithological and geochemical features provide some information about the climate changes that accompanied these events.

Abstract Image

查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
上列宁格勒勒拿河群(西伯利亚地台东南部)形成的岩石学和地球化学特征及古气候条件
摘要 在马来亚楚雅河右岸的一个地段研究了上列宁格勒勒拿河组(Є2-3vl)。利用 X 射线光谱荧光 (XRF) 分析法测定了样品中主要氧化物和一些微量元素(铬、钒、镍、铜、锌、铷、锶、锆、钡、铀、钍、钇、铌和氯)的浓度。根据 XRF 分析结果,使用 MINLITH 软件确定了标准矿物成分。根据地球化学数据,剥蚀区风化特征(物理/化学风化和干旱/湿润风化)的变化区间被清晰地区分,并通过 Al2O3/K2O 和 Ln(Al2O3/Na2O)比值、V、Cu、Zn、Rb 和 Ni 的浓度以及标准矿物成分的变化加以固定。显然,在这种情况下,铬完全是通过风化过程迁移到盆地的,这标志着风力迁移强度增加的时期。在上勒拿古盆地的构造激活和逐渐隔离的条件下,所描述的岩石学和地球化学特征提供了一些有关伴随这些事件发生的气候变化的信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍: Moscow University Geology Bulletin  is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
期刊最新文献
Geochemical and Sanitary–Chemical Characteristics of Water Springs of Bogorodsky and Losino-Petrovsky Districts of Moscow Oblast Assessment of Transmissivity of the Weathered Upper Part of Horizontally Layered Bedrock Structure of the Quaternary Sheet in Petrozavodsk Bay of Lake Onega According to Seismoacoustics Experimental Evaluation of the Peatification Effect on the Phase Composition of Water in Frozen Soils of with Different Grain Size Distributions Crystal-Chemical Indicators of Specification of Oxocentered Tetrahedra in Divalent Lead Minerals
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1