我国红层岩溶与红层岩溶塌陷刍议
中国岩溶地区面积广阔,岩溶地貌和现象类型多样。其中我国南方地区红层中出现的岩溶现象较为特殊：可溶岩类型复杂,成岩作用差,溶蚀机理多样,还易风化崩解。近年来红层岩溶塌陷多有发生,成为一个不可回避的问题。文章对我国红层岩溶与红层岩溶塌陷研究现状进行了系统梳理。红层岩溶主要存在于以可溶物质胶结的或含碳酸盐岩砾石的红色沉积岩为主的地区。红层岩溶的特点可以概括为：（1）可溶岩类型复杂,溶蚀机理多样;（2）成岩作用差,力学强度低,易风化崩解;（3）与地质构造密切相关。红层岩溶地区不但会出现覆盖型岩溶区的土层塌陷,而且由于其特殊的岩溶作用还可能出现基岩塌陷。根据红层岩溶地区地质结构,其塌陷模式可概化为红层上...
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| Published in | 中国岩溶 Vol. 35; no. 1; pp. 67 - 73 |
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| Main Author | |
| Format | Journal Article |
| Language | Chinese |
| Published |
中国地质科学院岩溶地质研究所/中国地质科学院岩溶塌陷防治重点实验室,广西 桂林,541004
2016
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| Subjects | |
| Online Access | Get full text |
| ISSN | 1001-4810 |
| DOI | 10.11932/karst20160110 |
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| Abstract | 中国岩溶地区面积广阔,岩溶地貌和现象类型多样。其中我国南方地区红层中出现的岩溶现象较为特殊：可溶岩类型复杂,成岩作用差,溶蚀机理多样,还易风化崩解。近年来红层岩溶塌陷多有发生,成为一个不可回避的问题。文章对我国红层岩溶与红层岩溶塌陷研究现状进行了系统梳理。红层岩溶主要存在于以可溶物质胶结的或含碳酸盐岩砾石的红色沉积岩为主的地区。红层岩溶的特点可以概括为：（1）可溶岩类型复杂,溶蚀机理多样;（2）成岩作用差,力学强度低,易风化崩解;（3）与地质构造密切相关。红层岩溶地区不但会出现覆盖型岩溶区的土层塌陷,而且由于其特殊的岩溶作用还可能出现基岩塌陷。根据红层岩溶地区地质结构,其塌陷模式可概化为红层上覆松散层塌陷、红层溶洞顶板垮塌以及红层整体垮塌三类。今后有必要从红层溶蚀特点和红层岩溶塌陷模式出发,开展红层溶蚀对岩溶塌陷作用机理的专项研究,为红层地区岩溶塌陷地质灾害的风险评估和防治处理提供科学依据和技术支撑。 |
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| AbstractList | P642.25; 中国岩溶地区面积广阔,岩溶地貌和现象类型多样.其中我国南方地区红层中出现的岩溶现象较为特殊:可溶岩类型复杂,成岩作用差,溶蚀机理多样,还易风化崩解.近年来红层岩溶塌陷多有发生,成为一个不可回避的问题.文章对我国红层岩溶与红层岩溶塌陷研究现状进行了系统梳理.红层岩溶主要存在于以可溶物质胶结的或含碳酸盐岩砾石的红色沉积岩为主的地区.红层岩溶的特点可以概括为:(1)可溶岩类型复杂,溶蚀机理多样;(2)成岩作用差,力学强度低,易风化崩解;(3)与地质构造密切相关.红层岩溶地区不但会出现覆盖型岩溶区的土层塌陷,而且由于其特殊的岩溶作用还可能出现基岩塌陷.根据红层岩溶地区地质结构,其塌陷模式可概化为红层上覆松散层塌陷、红层溶洞顶板垮塌以及红层整体垮塌三类.今后有必要从红层溶蚀特点和红层岩溶塌陷模式出发,开展红层溶蚀对岩溶塌陷作用机理的专项研究,为红层地区岩溶塌陷地质灾害的风险评估和防治处理提供科学依据和技术支撑. 中国岩溶地区面积广阔,岩溶地貌和现象类型多样。其中我国南方地区红层中出现的岩溶现象较为特殊：可溶岩类型复杂,成岩作用差,溶蚀机理多样,还易风化崩解。近年来红层岩溶塌陷多有发生,成为一个不可回避的问题。文章对我国红层岩溶与红层岩溶塌陷研究现状进行了系统梳理。红层岩溶主要存在于以可溶物质胶结的或含碳酸盐岩砾石的红色沉积岩为主的地区。红层岩溶的特点可以概括为：（1）可溶岩类型复杂,溶蚀机理多样;（2）成岩作用差,力学强度低,易风化崩解;（3）与地质构造密切相关。红层岩溶地区不但会出现覆盖型岩溶区的土层塌陷,而且由于其特殊的岩溶作用还可能出现基岩塌陷。根据红层岩溶地区地质结构,其塌陷模式可概化为红层上覆松散层塌陷、红层溶洞顶板垮塌以及红层整体垮塌三类。今后有必要从红层溶蚀特点和红层岩溶塌陷模式出发,开展红层溶蚀对岩溶塌陷作用机理的专项研究,为红层地区岩溶塌陷地质灾害的风险评估和防治处理提供科学依据和技术支撑。 |
| Author | 贾龙 吴远斌 潘宗源 殷仁朝 蒙彦 管振德 |
| AuthorAffiliation | 中国地质科学院岩溶地质研究所／中国地质科学院岩溶塌陷防治重点实验室,广西桂林541004 |
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| Author_FL | WU Yuan-bin JIA Long PAN Zong-yuan YIN Ren-chao MENG Yan GUAN Zhen-de |
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| Copyright | Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| DOI | 10.11932/karst20160110 |
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| DocumentTitleAlternate | A review of the research on karst and sinkhole of red beds in China |
| DocumentTitle_FL | A review of the research on karst and sinkhole of red beds in China |
| EndPage | 73 |
| ExternalDocumentID | zgyr201601010 668857779 |
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| Keywords | 岩溶塌陷 red beds karst karst collapse 红层岩溶 Chinese red beds 红层塌陷 中国红层 red beds collapse |
| Language | Chinese |
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| Notes | Chinese red beds, red beds karst, karst collapse, red beds collapse JIA Long,WU Yuan-bin,PAN Zong-yuan, YIN Ren-chao, MENG Yan, GUAN Zhen -e （Institute of Karst Geology, CAGS / Key Laboratory of Karst Collapse Prevention, CAGS,Guilin, Guangxi 541004,China） 45-1157/P The karst area in China is spacious and the karst types are d red beds area of south China are special, ln the region, the occurrence of iverse. The karst phenomena in the karst collapse has become a problem that cannot be avoided in recent years. So it is necessary to make a systematic analysis of the present situation of the research on the red bed karst and associated karst collapses, particularly occur in red-bed area in the country. Red-bed karst mainly occurs in South China where the red clastic rocks are cemented with solu- ble substances or contain carbonate gravels. The characteristics of the karst red beds can be summarized as follows： 1） karst types are complex and their dissolution mechanisms are diverse; 2） the red rock is not fully ceme |
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| PublicationTitle | 中国岩溶 |
| PublicationTitleAlternate | Carsologica Sinica |
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| PublicationYear | 2016 |
| Publisher | 中国地质科学院岩溶地质研究所/中国地质科学院岩溶塌陷防治重点实验室,广西 桂林,541004 |
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| Snippet | 中国岩溶地区面积广阔,岩溶地貌和现象类型多样。其中我国南方地区红层中出现的岩溶现象较为特殊：可溶岩类型复杂,成岩作用差,溶蚀机理多样,还易风化崩解。近年来红层岩溶塌... P642.25; 中国岩溶地区面积广阔,岩溶地貌和现象类型多样.其中我国南方地区红层中出现的岩溶现象较为特殊:可溶岩类型复杂,成岩作用差,溶蚀机理多样,还易风化崩解.近年来红... |
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| SubjectTerms | 中国红层 岩溶塌陷 红层塌陷 红层岩溶 |
| Title | 我国红层岩溶与红层岩溶塌陷刍议 |
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