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淮北煤田奥陶系灰岩岩溶类型及陷落柱成因分析
引用本文:宋晓梅,张永泰,李全. 淮北煤田奥陶系灰岩岩溶类型及陷落柱成因分析[J]. 安徽理工大学学报(自然科学版), 1997, 0(3)
作者姓名:宋晓梅  张永泰  李全
作者单位:皖北矿务局,皖北矿务局
摘    要:对淮北煤田奥陶系灰岩不同时期岩溶洞穴发育条件及特征进行了分析,将其分为冲蚀型、潜蚀型、流入型及含水层型岩溶洞穴。根据层状沉积岩层的断裂力学机制及洞穴的再发育过程,提出了煤系地层陷落柱多期活动模式。

关 键 词:岩溶洞穴  陷落柱  多期活动模式

The type of karst and forming mechanics of the calumnar callapse of the ordovician system calcarenite in Hudibei Field
Song Xiaomei, Zhong Yongtai, Li quan. The type of karst and forming mechanics of the calumnar callapse of the ordovician system calcarenite in Hudibei Field[J]. Journal of Anhui University of Science and Technology:Natural Science, 1997, 0(3)
Authors:Song Xiaomei   Zhong Yongtai   Li quan
Affiliation:Song Xiaomei; Zhong Yongtai; Li quan(Dept. of Resources and Environment Engineering) (Wanbei coal mine bureau)
Abstract:Analyses the forming factor and feature of karst cave of the ordorician systemcalcarenite in Huaibei coal field in different times and divides the karst cave into erodecave phrealic cave, inflow cave and aquifer cave. Acording to the fracture mechanics oflayered sedimentary and reforming prosess of the cave, the auther puts foward the model of many cycle activte cause of 'formating of the carst calumar callapse in coal bearingstrata
Keywords:karst cave  collumnar collapse  model
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