商 · 地震山崩多灾难——漫步地震五千年(3)

商周期间的地震记载多在川西—陕甘交界地区,山体垮塌十分普遍。现代科学将之划分成4种主要形态:落石、崩塌、滑坡和泥石流,其中以地震致崩塌和滑坡的危害最大。具体地介绍了汶川、湔江、叠溪和磨西地震山崩的灾情,特别是王家岩滑坡的力学机制;分析了历史上滑坡、河流改道、堰塞湖溃坝三大次生灾害;说明在青藏高原的推挤作用下,该区岩体的反复破裂是致灾元凶。...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:地震科学进展 2023-01 (12), p.594
1. Verfasser: 冯锐
Format: Artikel
Sprache:chi ; eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue 12
container_start_page 594
container_title 地震科学进展
container_volume
creator 冯锐
description 商周期间的地震记载多在川西—陕甘交界地区,山体垮塌十分普遍。现代科学将之划分成4种主要形态:落石、崩塌、滑坡和泥石流,其中以地震致崩塌和滑坡的危害最大。具体地介绍了汶川、湔江、叠溪和磨西地震山崩的灾情,特别是王家岩滑坡的力学机制;分析了历史上滑坡、河流改道、堰塞湖溃坝三大次生灾害;说明在青藏高原的推挤作用下,该区岩体的反复破裂是致灾元凶。
doi_str_mv 10.19987/j.dzkxjz.2023-050
format Article
fullrecord <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_journals_3083981765</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3083981765</sourcerecordid><originalsourceid>FETCH-proquest_journals_30839817653</originalsourceid><addsrcrecordid>eNpjYJAyNNAztLS0MNfP0kupyq7IqtIzMjAy1jUwNWBh4DQysDTTNTe3MOBg4C0uzkwyMDU0Njc0NDHlZLB7OrVN4dB2hadzNryc0_5048anW1Y-XTLreeO-l7P2PWqYAkTP9qx-tnYpRMGTXVOe9jY_3bnl_Z4O4_d7OnkYWNMSc4pTeaE0N4Oym2uIs4duQVF-YWlqcUl8Vn5pUR5QKt7YwMLY0sLQ3MzUmDhVAJyQUw0</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>3083981765</pqid></control><display><type>article</type><title>商 · 地震山崩多灾难——漫步地震五千年(3)</title><source>DOAJ Directory of Open Access Journals</source><creator>冯锐</creator><creatorcontrib>冯锐</creatorcontrib><description>商周期间的地震记载多在川西—陕甘交界地区,山体垮塌十分普遍。现代科学将之划分成4种主要形态:落石、崩塌、滑坡和泥石流,其中以地震致崩塌和滑坡的危害最大。具体地介绍了汶川、湔江、叠溪和磨西地震山崩的灾情,特别是王家岩滑坡的力学机制;分析了历史上滑坡、河流改道、堰塞湖溃坝三大次生灾害;说明在青藏高原的推挤作用下,该区岩体的反复破裂是致灾元凶。</description><identifier>ISSN: 2096-7780</identifier><identifier>DOI: 10.19987/j.dzkxjz.2023-050</identifier><language>chi ; eng</language><publisher>Beijing: Editorial Office of Progress in Earthquake Sciences</publisher><subject>Avalanches ; Dam failure ; Debris flow ; Disasters ; Dynasties ; Earthquakes ; Landslides ; Landslides &amp; mudslides ; Rocks ; Seismic activity ; Water diversion</subject><ispartof>地震科学进展, 2023-01 (12), p.594</ispartof><rights>2023. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,861,27905,27906</link.rule.ids></links><search><creatorcontrib>冯锐</creatorcontrib><title>商 · 地震山崩多灾难——漫步地震五千年(3)</title><title>地震科学进展</title><description>商周期间的地震记载多在川西—陕甘交界地区,山体垮塌十分普遍。现代科学将之划分成4种主要形态:落石、崩塌、滑坡和泥石流,其中以地震致崩塌和滑坡的危害最大。具体地介绍了汶川、湔江、叠溪和磨西地震山崩的灾情,特别是王家岩滑坡的力学机制;分析了历史上滑坡、河流改道、堰塞湖溃坝三大次生灾害;说明在青藏高原的推挤作用下,该区岩体的反复破裂是致灾元凶。</description><subject>Avalanches</subject><subject>Dam failure</subject><subject>Debris flow</subject><subject>Disasters</subject><subject>Dynasties</subject><subject>Earthquakes</subject><subject>Landslides</subject><subject>Landslides &amp; mudslides</subject><subject>Rocks</subject><subject>Seismic activity</subject><subject>Water diversion</subject><issn>2096-7780</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNpjYJAyNNAztLS0MNfP0kupyq7IqtIzMjAy1jUwNWBh4DQysDTTNTe3MOBg4C0uzkwyMDU0Njc0NDHlZLB7OrVN4dB2hadzNryc0_5048anW1Y-XTLreeO-l7P2PWqYAkTP9qx-tnYpRMGTXVOe9jY_3bnl_Z4O4_d7OnkYWNMSc4pTeaE0N4Oym2uIs4duQVF-YWlqcUl8Vn5pUR5QKt7YwMLY0sLQ3MzUmDhVAJyQUw0</recordid><startdate>20230101</startdate><enddate>20230101</enddate><creator>冯锐</creator><general>Editorial Office of Progress in Earthquake Sciences</general><scope>AFKRA</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>HCIFZ</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope></search><sort><creationdate>20230101</creationdate><title>商 · 地震山崩多灾难——漫步地震五千年(3)</title><author>冯锐</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-proquest_journals_30839817653</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi ; eng</language><creationdate>2023</creationdate><topic>Avalanches</topic><topic>Dam failure</topic><topic>Debris flow</topic><topic>Disasters</topic><topic>Dynasties</topic><topic>Earthquakes</topic><topic>Landslides</topic><topic>Landslides &amp; mudslides</topic><topic>Rocks</topic><topic>Seismic activity</topic><topic>Water diversion</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>冯锐</creatorcontrib><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><jtitle>地震科学进展</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>冯锐</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>商 · 地震山崩多灾难——漫步地震五千年(3)</atitle><jtitle>地震科学进展</jtitle><date>2023-01-01</date><risdate>2023</risdate><issue>12</issue><spage>594</spage><pages>594-</pages><issn>2096-7780</issn><abstract>商周期间的地震记载多在川西—陕甘交界地区,山体垮塌十分普遍。现代科学将之划分成4种主要形态:落石、崩塌、滑坡和泥石流,其中以地震致崩塌和滑坡的危害最大。具体地介绍了汶川、湔江、叠溪和磨西地震山崩的灾情,特别是王家岩滑坡的力学机制;分析了历史上滑坡、河流改道、堰塞湖溃坝三大次生灾害;说明在青藏高原的推挤作用下,该区岩体的反复破裂是致灾元凶。</abstract><cop>Beijing</cop><pub>Editorial Office of Progress in Earthquake Sciences</pub><doi>10.19987/j.dzkxjz.2023-050</doi></addata></record>
fulltext fulltext
identifier ISSN: 2096-7780
ispartof 地震科学进展, 2023-01 (12), p.594
issn 2096-7780
language chi ; eng
recordid cdi_proquest_journals_3083981765
source DOAJ Directory of Open Access Journals
subjects Avalanches
Dam failure
Debris flow
Disasters
Dynasties
Earthquakes
Landslides
Landslides & mudslides
Rocks
Seismic activity
Water diversion
title 商 · 地震山崩多灾难——漫步地震五千年(3)
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-20T13%3A42%3A36IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=%E5%95%86%20%C2%B7%20%E5%9C%B0%E9%9C%87%E5%B1%B1%E5%B4%A9%E5%A4%9A%E7%81%BE%E9%9A%BE%E2%80%94%E2%80%94%E6%BC%AB%E6%AD%A5%E5%9C%B0%E9%9C%87%E4%BA%94%E5%8D%83%E5%B9%B4%EF%BC%883%EF%BC%89&rft.jtitle=%E5%9C%B0%E9%9C%87%E7%A7%91%E5%AD%A6%E8%BF%9B%E5%B1%95&rft.au=%E5%86%AF%E9%94%90&rft.date=2023-01-01&rft.issue=12&rft.spage=594&rft.pages=594-&rft.issn=2096-7780&rft_id=info:doi/10.19987/j.dzkxjz.2023-050&rft_dat=%3Cproquest%3E3083981765%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=3083981765&rft_id=info:pmid/&rfr_iscdi=true