俄罗斯阿尔泰地区库切拉湖冰川粘土气候变化与地震事件档案资料

Pub Date : 2020-09-23 DOI:10.5800/gt-2020-11-3-0495
A. Darin, G. Chu, Q. Sun, V. Babich, I. Kalugin, T. Markovich, V. S. Novikov, F. Darin, Y. Rakshun
{"title":"俄罗斯阿尔泰地区库切拉湖冰川粘土气候变化与地震事件档案资料","authors":"A. Darin, G. Chu, Q. Sun, V. Babich, I. Kalugin, T. Markovich, V. S. Novikov, F. Darin, Y. Rakshun","doi":"10.5800/gt-2020-11-3-0495","DOIUrl":null,"url":null,"abstract":". Core samples taken from the bottom sediments of the glacial Lake Kucherla (Gorny Altai, Russia) clearly show annual layers represented by glacial clays. In our study, age-depth modeling is based the varve chronology and Cs-137, Pb-210 and C-14 isotope data. Our model is a highly accurate and reliable demonstration of the annual sedimentation history within the past 1400 years. The time series of geochemical indicators of climate change were obtained by synchrotron radiation micro X-ray fluorescence (SR-µXRF) core scanning. Instrumental meteorological observations from 1940 to 2016 were used to construct transfer functions for the average annual temperatures and atmospheric precipitation amounts. A geochemical trace of a catastrophic seismic event, the Mongolian earthquake of 1761, was found in the cross-section of the bottom sediments.","PeriodicalId":0,"journal":{"name":"","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2020-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Archive data on climate changes and seismic events in glacial clays of Lake Kucherla (Altai region, Russia)\",\"authors\":\"A. Darin, G. Chu, Q. Sun, V. Babich, I. Kalugin, T. Markovich, V. S. Novikov, F. Darin, Y. Rakshun\",\"doi\":\"10.5800/gt-2020-11-3-0495\",\"DOIUrl\":null,\"url\":null,\"abstract\":\". Core samples taken from the bottom sediments of the glacial Lake Kucherla (Gorny Altai, Russia) clearly show annual layers represented by glacial clays. In our study, age-depth modeling is based the varve chronology and Cs-137, Pb-210 and C-14 isotope data. Our model is a highly accurate and reliable demonstration of the annual sedimentation history within the past 1400 years. The time series of geochemical indicators of climate change were obtained by synchrotron radiation micro X-ray fluorescence (SR-µXRF) core scanning. Instrumental meteorological observations from 1940 to 2016 were used to construct transfer functions for the average annual temperatures and atmospheric precipitation amounts. A geochemical trace of a catastrophic seismic event, the Mongolian earthquake of 1761, was found in the cross-section of the bottom sediments.\",\"PeriodicalId\":0,\"journal\":{\"name\":\"\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0,\"publicationDate\":\"2020-09-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5800/gt-2020-11-3-0495\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5800/gt-2020-11-3-0495","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

摘要

. 从库切拉冰川湖(戈尔尼阿尔泰,俄罗斯)底部沉积物中提取的岩心样本清楚地显示出以冰川粘土为代表的年层。在我们的研究中,年龄深度建模是基于阀门年代学和Cs-137、Pb-210和C-14同位素数据。我们的模型对过去1400年的年沉积历史进行了高度精确和可靠的论证。通过同步辐射微x射线荧光(SR-µXRF)岩心扫描,获得了气候变化地球化学指标的时间序列。利用1940 - 2016年的仪器气象观测资料,构建了年平均气温和大气降水量的传递函数。在底部沉积物的横截面上发现了1761年蒙古地震这一灾难性地震事件的地球化学痕迹。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
分享
查看原文
Archive data on climate changes and seismic events in glacial clays of Lake Kucherla (Altai region, Russia)
. Core samples taken from the bottom sediments of the glacial Lake Kucherla (Gorny Altai, Russia) clearly show annual layers represented by glacial clays. In our study, age-depth modeling is based the varve chronology and Cs-137, Pb-210 and C-14 isotope data. Our model is a highly accurate and reliable demonstration of the annual sedimentation history within the past 1400 years. The time series of geochemical indicators of climate change were obtained by synchrotron radiation micro X-ray fluorescence (SR-µXRF) core scanning. Instrumental meteorological observations from 1940 to 2016 were used to construct transfer functions for the average annual temperatures and atmospheric precipitation amounts. A geochemical trace of a catastrophic seismic event, the Mongolian earthquake of 1761, was found in the cross-section of the bottom sediments.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
×
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
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
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 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信