Crust Macrofracturing as the Evidence of the Last Deglaciation

Author:

Aleshin Igor1,Kholodkov Kirill1,Kozlovskaya Elena,Malygin Ivan1

Affiliation:

1. Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences

Abstract

Abstract Machine learning methods were applied to reconsider the results of several passive seismic experiments in Finland. We created datasets from different stages of the receiver function technique and processed them with one of basic machine learning algorithms. All the results were obtained uniformly with the k-nearest neighbors algorithm. The first result is the Moho depth map of the region. Another result is the delineation of the near-surface low S-wave velocity layer. There are three such areas in the Northern, Southern, and central parts of the region. The low S-wave velocity in the Northern and Southern areas can be linked to the geological structure. However, we attribute the central low S-wave velocity area to a large number of water-saturated cracks in the upper 1-5 km. Analysis of the structure of this area leads us to the conclusion that macrofracturing was caused by the last deglaciation.

Publisher

Research Square Platform LLC

Reference37 articles.

1. Bock, G ünter and Achauer, Ulrich and Alinaghi, A. and Ansorge, J. and Bruneton, M. and Friederich, W. and Grad, M. and Guterch, A. and Hjelt, S.-E and Hyv önen, T. and Ikonen, J.-P and Kissling, Edi (2001) Seismic probing of Fennoscandian Lithosphere. Eos, Transactions American Geophysical Union 82: 621-621 https://doi.org/10.1029/01EO00356, 12

2. {Kozlovskaya}, E. and {Poutanen}, M. and {Polenet/Lapnet Working Group} (2006) {POLENET/LAPNET- a multidisciplinary geophysical experiment in northern Fennoscandia during IPY 2007-2008}. Provided by the SAO/NASA Astrophysics Data System, https://ui.adsabs.harvard.edu/abs/2006AGUFM.S41A1311K, S41A-1311, S41A-1311, December, 2006, AGU Fall Meeting Abstracts, 1219 Gravity anomalies and Earth structure (0920, 7205, 7240), 1295 Integrations of techniques, 7207 Core (1212, 1213, 8124), 7208 Mantle (1212, 1213, 8124), 7218 Lithosphere (1236)

3. Bruneton, Marianne and Farra, V éronique and Pedersen, Helle Anette (2002) {Non-linear surface wave phase velocity inversion based on ray theory}. Geophysical Journal International 151(2): 583-596 https://doi.org/10.1046/j.1365-246X.2002.01796.x, https://academic.oup.com/gji/article-pdf/151/2/583/5871439/151-2-583.pdf, https://doi.org/10.1046/j.1365-246X.2002.01796.x, 0956-540X, 11

4. Alinaghi, A. and Bock, G. and Kind, R. and Hanka, W. and Wylegalla, K. and TOR and SVEKALAPKO Working Groups (2003) {Receiver function analysis of the crust and upper mantle from the North German Basin to the Archaean Baltic Shield}. Geophysical Journal International 155(2): 641-652 https://doi.org/10.1046/j.1365-246X.2003.02075.x, https://academic.oup.com/gji/article-pdf/155/2/641/1631408/155-2-641.pdf, https://doi.org/10.1046/j.1365-246X.2003.02075.x, 0956-540X, 11

5. Aleshin, Igor and Kosarev, Grigoriy and Riznichenko, O. and Sanina, Irina (2006) Crustal Velocity Structure Under the {RUKSA} Seismic Array ({Karelia}, {Russia}). Russian Journal of Earth Sciences 8: 1-8 https://doi.org/10.2205/2006ES000194, 03

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3