许志琴^1,2,,
吴忠良³,
李海兵²,
李丽⁴
1. 南京大学地球科学与工程学院, 南京 210046
2. 自然资源部深地动力学重点实验室, 中国地质科学院地质研究所, 北京 100037
3. 中国地震局地震预测研究所, 北京 100036
4. 中国地震局地球物理研究所, 北京 100081

基金项目: 国家科技专项"汶川地震断裂带科学钻探"和国家自然科学基金项目（41330211）资助


详细信息

作者简介: 许志琴, 女, 1941年生, 中国科学院院士, 南京大学地球科学与工程学院教授, 汶川地震断裂带科学钻探工程首席科学家, 长期从事青藏高原和中国造山带研究.E-mail:3077864156@qq.com

中图分类号: P313;P541

收稿日期:2018-04-17
修回日期:2018-04-22
上线日期:2018-05-05

The most rapid respond to a large earthquake—the Wenchuan earthquake Fault Scientific Drilling Project

XU ZhiQin^1,2,,
WU ZhongLiang³,
LI HaiBing²,
LI Li⁴
1. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210046, China
2. Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China
4. Institute of Geophysics, China Earthquake Administration, Beijing 100081, China


MSC: P313;P541

--> Received Date: 17 April 2018
Revised Date: 22 April 2018
Available Online: 05 May 2018


摘要
摘要:2008年5月12日汶川大地震之后，在青藏高原东缘龙门山地区实施了汶川地震断裂带科学钻探，这是目前世界上最快回应大地震的科学钻探，为地学家探索地震成因机制提供了极好的机遇.汶川地震断裂带科学钻探工程（WFSD）沿产生同震地表破裂的两条断裂带——龙门山的映秀—北川断裂和灌县—安县断裂共实施了6口科学群钻.其目标在于对钻孔的岩心、岩屑和流体样品进行多学科观察、测试和研究，揭示汶川地震断裂带的深部物质组成、结构、产出以及构造属性；探索地震过程中的岩石物理和化学行为、能量状态与破裂演化过程；认识汶川地震发生的应力环境、巨大的地震破裂产生及传播原因、地下流体在地震的孕育、发生、停止过程中的作用，从而检验和深入理解地震断裂发震机理.目前，汶川科钻项目已取得的部分重要成果如下：（1）查明了汶川地震断裂带结构、组成；（2）揭示了汶川地震过程中"热增压"为重要断裂弱化机制，提出断裂带内石墨可作为判断大地震发生的标志；（3）发现目前世界上最低的断层摩擦系数，并首次记录到大震后断裂带快速愈合信息；（4）重建龙门山的构造格架，提出汶川大地震发生的新的成因模式；（5）通过对汶川地震余震的精确定位、钻孔附近的地震台阵观测，确定了地震活动与龙门山断裂带不同区段的空间关系；揭示断裂带深部流体特征与地震活动的关系，为确定大震孕育过程提供深部流体活动行为的科学依据.
关键词: 龙门山构造带/
WFSD/
汶川地震10周年/
地震机制/
构造格架

Abstract:After the devastating Wenchuan earthquake on May 12, 2008, the Wenchuan earthquake Fault Scientific Drilling project (WFSD) was carried out in the eastern Tibetan Plateau, which is the most rapid scientific drilling response to large earthquakes in the world. The WFSD project provides an excellent opportunity for geoscientists to explore the formation mechanism of earthquakes. In total, 6 drilling boreholes were drilled along the Yingxiu-Beichuan and Guanxian-Anxian faults (Longmen Shan, China), which both ruptured during the Wenchuan earthquake. The WFSD project aims to reveal the composition, structure, morphology and tectonic properties of the Wenchuan earthquake fault zone at deep depths based on multi-disciplinary observations, measurements and analyses, to explore the physical and chemical behavior of the faults, their energy states, as well as their rupture processes during the Wenchuan earthquake. Thus, we aim to further understand the stress condition, the causes of nucleation and propagation of the rupture, the role of fluid in earthquake nucleation, propagation, and cessation, and the seismogenic mechanism of seismic faults. So far, some important research results have been achieved: (1) We know the structure of the Wenchuan earthquake fault zone. (2) We suggested that thermal pressurization was an important fault weakening mechanism during the Wenchuan earthquake, and that graphite in fault zone can be considered as an indicator to determine the occurrence of large earthquakes. (3) We obtained the lowest fault's frictional coefficient in the world and recorded the information about fault healing quickly after this large earthquake for the first time. (4) We reconstructed the tectonic framework of the Longmen Shan and presented a new formation model of the Wenchuan earthquake. (5) We determined the spatial relationship between seismic activity and the different sections of the Longmen Shan thrust belt by accurately locating the aftershocks of the Wenchuan earthquake and by observing the seismic array near the boreholes, and revealed the relationship between the characteristics of fluid and seismic activities in the fault zone at deep depth, which provides the scientific basis for determining the formation process of large earthquakes.
Key words:Longmen Shan fault zone/
WFSD/
The 10th anniversary of the Wenchuan earthquake/
Earthquake mechanism/
Tectonic framework



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