Disturbed granite identification by integrating rock mass geophysical properties

被引:7
作者
Lin, Daming [1 ]
Yuan, Renmao [2 ]
Lin, Xiaoling [3 ]
Lin, Xuechun [4 ]
Lou, Chonghua [4 ]
Cai, Yanyan [5 ]
Yu, Jin [5 ]
Qiu, Renke [4 ]
Su, Xingju [4 ]
Wang, Hui [1 ]
机构
[1] Minist Transport, Res Inst Highway, Beijing 100088, Peoples R China
[2] China Earthquake Adm, Key Lab Act Tecton & Volcanoes, Inst Geol, Beijing 100049, Peoples R China
[3] China Univ Geosci Beijing, Sch Engn & Technol, Beijing 100088, Peoples R China
[4] Supervis Bur Traff Construct Qual & Safety Fujian, Fuzhou 350011, Peoples R China
[5] Huaqiao Univ, Sch Civil Engn, Xiamen 361021, Peoples R China
基金
中国国家自然科学基金;
关键词
Seismic velocity; RCI; Electrical resistivity; RQD; Granite;
D O I
10.1016/j.ijrmms.2020.104596
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Granite is exposed across 9% of China, and many major infrastructures are located in granitic areas because of the intact structure and high compressive strength of granite. Therefore, the identification of disturbed granite by integrating rock mass properties is important for construction safety. In this paper, the authors utilize data from 278 shallow boreholes and 12 geophysical exploration lines in South China and establish a 3-D geological-geophysical model. A quantitative relationship between the disturbed rock mass structure and rock core index (RCI) is then established. An empirical relationship between the electrical resistivity and the seismic velocity of the disturbed granite at the China Spallation Neutron Source (CSNS) site is also obtained. This research enhances the quantitative characterization of disturbed granite, especially disintegrated laminated granite, using rock mass geophysical parameters.
引用
收藏
页数:9
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