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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

文章导航 > 地质力学学报  > 2024 >  30(2): 181-188
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
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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
shu

活动构造与强震：专辑序言

doi: 10.12090/j.issn.1006-6616.20243002
  • 1.

    中国地质科学院地质力学研究所，北京 100081

  • 2.

    中山大学地球科学与工程学院，广东 珠海 519082

  • 3.

    中国地质大学(北京)地球科学与资源学院，北京 100083

  • 4.

    中国地震局地质研究所，北京 100029

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

  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai 519082, Guangdong, China

  • 3.

    School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China

  • 4.

    Institute of geology, China Earthquake Administration, Beijing 100029, China

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
  • 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。

     

    Abstract: Active tectonics is not only the manifestation of the latest crustal activity but also the leading cause of strong earthquakes. With its complex active tectonic system, China has become an area with particularly severe seismic activity and related hazards worldwide. Therefore, a deep understanding of active tectonic characteristics and the occurrence patterns of strong earthquakes in China can help scientifically prevent or mitigate the risk of seismic disasters in urban planning and major engineering construction projects. In order to timely exchange the latest achievements in the field of active tectonics and strong earthquakes, this special issue on Active Tectonics and Strong Earthquakes selected 12 representative papers, mainly covering six different fields, including the earthquake-controlling process of active tectonics, paleoearthquakes, surveying and detection of active faults, seismic geological hazards, application of remote sensing technology and reservoir-induced earthquakes. Based on the new achievements of this issue and the research trends in related fields at home and abroad, it is suggested that future research on active tectonics and strong earthquakes should focus on four aspects: (1) comprehensive understanding of regional seismic hazards from the perspective of active tectonic evolution and active fault systems; (2) quantitative and refined field investigations of active tectonics; (3) application of high-precision remote sensing and various dating techniques continuously expanding the scope and timing of paleoearthquake research; (4) human-induced earthquakes.

     

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  • 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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