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辽宁本溪晶花洞碳酸钙沉积物颜色多样性分析
引用本文:秦亚,程新民,常建平,李泽峰.辽宁本溪晶花洞碳酸钙沉积物颜色多样性分析[J].中国岩溶,2011,30(3):354-358.
作者姓名:秦亚  程新民  常建平  李泽峰
作者单位:1. 吉林大学地球科学学院,吉林长春,130061
2. 青海省第三地质矿产勘查院,青海西宁,810008
基金项目:国家自然科学基金项目(40973060)、中国科学院战略性先导科技专项重大课题(XDA05070400)、贵州省社会发展科技攻关计划项目(SY[2010]3043)
摘    要:辽宁本溪晶花洞发育于中奥陶统马家沟组(O2m)中厚层白云质灰岩中,洞内碳酸钙沉积物具有白色、黄色、肉红色、浅蓝色和黑褐色等多种原生色彩。在洞穴考察的基础上,通过对围岩和洞穴碳酸钙沉积物X荧光分析以及显微镜薄片鉴定,认为洞穴中自色的次生化学沉积物主要由质纯的CaCO3形成;浅蓝色、黑褐色的形成则多由沉积物含有铜、锶和锰、锌所致;而黄色、红色则为不同环境下铁、锰等变价元素所产生。

关 键 词:岩溶洞穴  碳酸钙沉积物  颜色多样性  致色物质  色彩成因  晶花洞  辽宁本溪
收稿时间:4/3/2011 12:00:00 AM

A study on the color variety of speleothems Jinghua Cave in Benxi, Liaoning Province
QIN Y,CHENG Xin-min,CHANG Jian-ping and LI Ze-feng.A study on the color variety of speleothems Jinghua Cave in Benxi, Liaoning Province[J].Carsologica Sinica,2011,30(3):354-358.
Authors:QIN Y  CHENG Xin-min  CHANG Jian-ping and LI Ze-feng
Institution:College of Earth Sciences, Jilin University;College of Earth Sciences, Jilin University;College of Earth Sciences, Jilin University;The Third Institution of Qinghai Geological Mineral Prospecting
Abstract:Jinghua Cave is developed in thick-bedded limestone of the Middle Ordovician Majiagou Formation in Benxi, Liaoning. Speleothems in the cave have many primary colors, such as white, yellow, red, blue and black. On the basis of research on the cave, X RF analysis and thin-section identification under the microscope have done. It is confirmed that the white color comes from pure CaCO3, blue and black from Cu, Sr, Mn and Zn components in the speleothems, yellow and red from some elements like Fe and Mn with different valence under different conditions.
Keywords:karst cave  speleothem  color variety  colourant  cause of color  Jinghua Cave  Benxi in Liaoning Province
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