[1]谭艳,朱诚,吴立,等.广东丹霞山砂岩蜂窝状洞穴及白斑成因[J].山地学报,2015,(03):279.
　TAN Yan,ZHU Cheng,WU Li,et al.Geomophogensis on Sandstone Honeycombs and White Spot in the Mt. Danxiashan，Guangdong Province，South China[J].Mountain Research,2015,(03):279.
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广东丹霞山砂岩蜂窝状洞穴及白斑成因()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年03期
页码:
279
栏目:
山地研究
出版日期:
2015-06-01

文章信息/Info

Title:
Geomophogensis on Sandstone Honeycombs and White Spot in the Mt. Danxiashan，Guangdong Province，South China
作者:
谭艳;朱诚;吴立;孙伟;王晓翠;贾天骄;彭华;侯荣丰;
南京大学地理与海洋科学学院;安徽师范大学国土资源与旅游学院;中国科学院南京地理与湖泊研究所;中山大学地理科学与规划学院;丹霞山风景名胜区管理委员会;
Author(s):
TAN Yan; ZHU Cheng; WU Li; SUN Wei; WANG Xiaocui;  JIA Tianjiao; PENG Hua; HOU Rongfeng
1. School of Geographic and Oceanographic Science，Nanjing University，Nanjing 210093，Jiangsu，China； 2. College of Territorial Resources and Tourism，Anhui Normal University，Wuhu 241002，Anhui，China； 3. Nanjing Institute of Geography & Limnology，Chinese Academy of Sciences，Nanjing 210008，Jiangsu，China； 4. School of Geography and Planning，Sun Yat-sen University，510275，Guangzhou，China 5. Administrative Committee of Danxiashan Scenic Spot，Shaoguan 512300，Guangdong，China
关键词:
广东丹霞山; 砂岩; 成分分析; 蜂窝状洞穴; 白斑
Keywords:
Mt. Danxiashan; sandstone; component analysis; honeycombs; white spot
分类号:
P931
文献标志码:
A
摘要:
为研究广东韶关市丹霞山砂岩蜂窝状洞穴及白斑成因,对世界自然遗产地丹霞山景区内玉女拦江洞中采集的6个砂岩蜂窝状洞穴样品,以及在鸭麻岩地区采集的4个白斑样品,进行XRF和ICP-MS元素地球化学分析及岩石薄片偏光显微镜鉴定。结果表明,发育蜂窝状洞穴的砂岩体与其基岩砂岩体的成分含量相近,岩体内部成分差异不是蜂窝状洞穴的成因。综合分析认为,丹霞山砂岩蜂窝状洞穴的产生是岩石的矿物组成及结构、洞穴所在的地形条件、气候因素和蜂窝状洞穴所形成的微气候共同作用的结果。对白斑的元素分析结果显示,发育白斑的砂岩在成岩过程中,红色基岩形成于氧化环境,而白斑形成于还原环境中,赤铁矿被还原形成白斑。
Abstract:
Abundant typical sandstone morphologic shapes developed in Mt. Danxiashan. We collected six samples of sandstone honeycombs in Yunülanjiang Cave and four samples of white spots in Yamayan to do component analysis (XRF and ICP-MS) with the purpose of explaining their genesis. The results indicate that the component contents of samples in honeycombs and bedrock are similar so that there is no direct relationship between lithological differences and honeycomb’s formation. The comprehensive analysis reveals that honeycombs are the result of physical weathering. And the rock structure，topography，climate and cavern microclimate are important influencing factors in the formation process of honeycombs. In the discussion of sandstone white spot，reducing conditions prevail in the process and some minerals are dissolved. Reduction of Fe making the color change from red to white with water percolating through the rock，thereby forming a white spot on the surface.

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备注/Memo

备注/Memo:
收稿日期(Received date)：2014-04-12；改回日期(Accepted)：2014-05-04。
基金项目(Foundation item)：国家自然科学
基金项目（41371204，41171163）；国家科技基础性专项重点项目（2013FY111900）。[National Natural Science Foundation of China(41371204, 41171163)；National science and technology basic special key projects(2013FY111900).]
作者简介（Biography）：谭艳（1990-），女，宁夏石嘴山人，硕士研究生，主要研究方向为地貌与第四纪环境演变。[Tan Yan(1990-), female, born in Shizuishan of Ningxia, postgraduate student, in Geomorphology and quaternary environmental change analysis. ] E-mail: tanyan9001@126.com *
通信作者(Corresponding author)：朱诚[Zhu Cheng]，E-mail: zhuchengnj@126.com；吴立[Wu Li]，E-mail: jedi-wuli@163.com
更新日期/Last Update: 1900-01-01