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活动构造与强震:专辑序言

吴中海 郑文俊 任俊杰 任治坤

吴中海, 郑文俊, 任俊杰, 等, 2024. 活动构造与强震:专辑序言. 地质力学学报, 30 (2): 181-188. DOI: 10.12090/j.issn.1006-6616.20243002
引用本文: 吴中海, 郑文俊, 任俊杰, 等, 2024. 活动构造与强震:专辑序言. 地质力学学报, 30 (2): 181-188. DOI: 10.12090/j.issn.1006-6616.20243002
WU Zhonghai, ZHENG Wenjun, REN Junjie, et al., 2024. Active tectonics and strong earthquakes: A preface for the special issue. Journal of Geomechanics, 30 (2): 181-188. DOI: 10.12090/j.issn.1006-6616.20243002
Citation: WU Zhonghai, ZHENG Wenjun, REN Junjie, et al., 2024. Active tectonics and strong earthquakes: A preface for the special issue. Journal of Geomechanics, 30 (2): 181-188. DOI: 10.12090/j.issn.1006-6616.20243002

活动构造与强震:专辑序言

doi: 10.12090/j.issn.1006-6616.20243002
基金项目: 

中国地质调查局地质调查项目 DD20242319

中国地质调查局地质调查项目 DD20230014

国家自然科学基金联合基金项目 U2002211

国家自然科学基金联合基金项目 U2139201

西藏自治区第1次全国自然灾害综合风险普查项目(2022年地震灾害部分) XZLX-BMC-2022-053

详细信息
  • 中图分类号: P315

Active tectonics and strong earthquakes: A preface for the special issue

Funds: 

the Geological Survey Project of the China Geological Survey DD20242319

the Geological Survey Project of the China Geological Survey DD20230014

the Joint Fund of the National Natural Science Foundation of China U2002211

the Joint Fund of the National Natural Science Foundation of China U2139201

the First National Natural Disaster Comprehensive Risk Survey Project of Xizang Autonomous Region XZLX-BMC-2022-053

  • 摘要: 活动构造既是地壳最新活动的表现,也是导致强震的主要根源。中国大陆因发育了复杂的活动构造系统,成为世界上强震活动及相关灾害特别严重的地区。因此,深入认识中国大陆的活动构造特征与强震发生规律,有助于在城镇规划和重大工程建设中科学防范或规避强震灾害风险。为了及时交流活动构造与强震研究领域的最新成果,此期专辑优选了代表性论文12篇,主要涵盖了活动构造控震、古地震、活动断裂调查与探测、地震地质灾害、遥感技术应用和水库诱发地震共6个不同领域的研究进展。综合此期专辑的新成果和国内外相关领域的研究动态,建议活动构造与强震研究应关注4个方面的动态进展,包括:从活动构造演化及活动断裂体系角度更全面地认识区域强震的危险性;活动构造已步入定量化与精细化调查研究阶段;高精度遥感和多种定年技术的应用正在不断扩展古地震研究的范围和时限;人类活动诱发地震问题。

     

  • 图  1  活断层的典型地貌标志与地质剖面上的断错标志及时代分类示意图(吴中海,2022)

    Figure  1.  Schematic diagram of the geomorphologic marks of surface active faults (a-c) and the characteristics of the age classification of active fault based on the marks of offset Quaternary deposits(Wu, 2022)

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