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安徽巢湖地区石炭纪炉渣状灰岩的成因研究
引用本文:徐继山,马学军,马润勇,李注苍,付恒阳.安徽巢湖地区石炭纪炉渣状灰岩的成因研究[J].地层学杂志,2012(3):672-678.
作者姓名:徐继山  马学军  马润勇  李注苍  付恒阳
作者单位:长安大学地质工程与测绘学院;中国地质调查局水文地质环境地质调查中心;西部矿产资源与地质工程教育部重点实验室;长安大学地球科学与资源学院
基金项目:华北平原地裂缝调查与评价(No.1212010914019)项目资助
摘    要:安徽巢湖地区炉渣状灰岩的成因主要有三种假说,即风化作用、生物扰动、地震作用等三种假说从沉积过程的不同阶段做出相异解释,恰好说明了炉渣状灰岩的成因是多因素、多阶段的。在地质勘察的基础上,结合"地质—生物—环境"三者之间的相互影响探讨炉渣状灰岩的综合成因。

关 键 词:岩石地层  炉渣状灰岩  地质作用  生物扰动  环境变迁  沉积作用  石炭纪  巢湖地区  安徽

ON THE ORIGIN OF CARBONIFEROUS SLAP-LIKE LIMESTONE IN CHAOHU,ANHUI PROVINCE
XU Ji-shan,MA Xue-jun,MA Run-yong,LI Zhu-cang,and FU Heng-yang.ON THE ORIGIN OF CARBONIFEROUS SLAP-LIKE LIMESTONE IN CHAOHU,ANHUI PROVINCE[J].Journal of Stratigraphy,2012(3):672-678.
Authors:XU Ji-shan  MA Xue-jun  MA Run-yong  LI Zhu-cang  and FU Heng-yang
Institution:1) 1) College of Geology Engineering and Geomatics,Chang’an University,Xi’an 710054;2) Center for Hydrogeology and Environmental Geology,CGS,Baoding 071051;3) Key Laboratory of Western Mineral Resources and Geological Engineering Ministry of Education,Xi’an 710054;4) College of Earth Science and Resources,Chang’an University,Xi’an 710054
Abstract:The origin of Carboniferous slag-like limestone in Chaohu,Anhui Province,has drawn wide attention and discussion.Three hypotheses have been proposed,relating its origin to chemical weathering,bioturbation,and seismic activities.These hypotheses emphasize geological processes in different sedimentary and diagenetic stages.On the basis of geological survey,we consider that a combination of geological,biological,and environmental factors have contributed to the formation of the slap-like limestone in Chaohu,Anhui Province.
Keywords:lithostratigraphy  slap-like limestone  geologic function  bioturbation  environmental transition  sedimentation  Carboniferous  Chaohu area  Anhui
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