• 责任者：Li Xianglong (Department of Engineering ; China University of Geosciences ; Wuhan 430074 ; China) ; Tang Huiming
• 刊名：Coal Geology & Exploration
• 出版年：2011
• 卷期：39(6)
• 关键词：岩质滑坡 ; rockslides ; 地震效应 ; seismic effects ; 四川 ; Sichuan Province
• 页码：p.48-53
• 图表：4 illus., 1 table, 8 refs.
• 分类号：1702
• issnNo：ISSN1001-1986
• isbnNo：CN61-1155/P

A new definition named sliding-surface breccia was brought according to the characteristics and mineral identification of this special rock shell. By analyzing the mechanism of fast rock granular cementation, it is proved that under the severe earthquake and certain specific geological and topographical conditions, the temperature in the sliding zone can rise to meet the required temperature under which rock particles in the sliding zone can be conglomerated by ferruginous cementation. In addition, this temperature is far lower than the mineral melting temperature of rocks.