COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

朱诚; 宋友桂

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名

邮箱

手机号码

标题

留言内容

验证码

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

朱诚,
宋友桂

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

摘要: The data of Fe³⁺/Fe²⁺ show that the lowest annual air temperature of the Lushan,Huangshan and Tianmu mountains was not below 0℃, therefore, glacier couldn't develop in there regions. According to palaeomagnetic test combined with the phenomenon of reticulate pattern ground and lithologic identification, the authors elaborate that the “Poyang moraine” is mainly the fluvial sediments of the early period of the Middle Pleistocene. It was formed by transposition of the ancient Ganjiang River under the humid hot climate. For CM image, the Dajiaochang profile of the Lushan Mountain is very similar to periglacial and the debris flow deposits, but the profile of Jiangpochang and Yaoshaling have many kinds of geneses, i.e., debris flow, water debris flow and alluvial etc. In the south piedmont of the Huangshan Mountain, slope gravity and slope seasonal running water transportantion are mainly deposit factors. In the “glacial varve” of the Denglongqiao profile of the Tianmu Mountain, its CaO and Na₂O content is lower than the nonglacial varve, the fact shows that it has the features of the violent leaching, weathering and nonglacial action.
- Lushan Mountain /
- Huangshan Mountain /
- Tianmu Mountain /
- Quaternary deposit environment
Abstract: The data of Fe³⁺/Fe²⁺ show that the lowest annual air temperature of the Lushan,Huangshan and Tianmu mountains was not below 0℃, therefore, glacier couldn't develop in there regions. According to palaeomagnetic test combined with the phenomenon of reticulate pattern ground and lithologic identification, the authors elaborate that the “Poyang moraine” is mainly the fluvial sediments of the early period of the Middle Pleistocene. It was formed by transposition of the ancient Ganjiang River under the humid hot climate. For CM image, the Dajiaochang profile of the Lushan Mountain is very similar to periglacial and the debris flow deposits, but the profile of Jiangpochang and Yaoshaling have many kinds of geneses, i.e., debris flow, water debris flow and alluvial etc. In the south piedmont of the Huangshan Mountain, slope gravity and slope seasonal running water transportantion are mainly deposit factors. In the “glacial varve” of the Denglongqiao profile of the Tianmu Mountain, its CaO and Na₂O content is lower than the nonglacial varve, the fact shows that it has the features of the violent leaching, weathering and nonglacial action.
- Lushan Mountain /
- Huangshan Mountain /
- Tianmu Mountain /
- Quaternary deposit environment

[1]	Rong WANG, Xueyan ZHAO. Can Multiple Livelihood Interventions Improve Livelihood Resilience of Out-of-poverty Farmers in Mountain Areas? A Case Study of Longnan Mountain Area, China . Chinese Geographical Science, 2023, 33(5): 898-916. doi: 10.1007/s11769-023-1384-7
[2]	Shiman HUANG, Qingwu HU, Shaohua WANG, Haidong LI. Ecological Risk Assessment of World Heritage Sites Using RS and GIS: A Case Study of Huangshan Mountain, China . Chinese Geographical Science, 2022, 32(5): 808-823. doi: 10.1007/s11769-022-1302-4
[3]	ZHANG Yi. Effect of Aspect on Climate Variation in Mountain Ranges of Shennongjia Massif, Central China . Chinese Geographical Science, 2018, 28(1): 74-85. doi: 10.1007/s11769-017-0917-3
[4]	SUN Feixiang, LYU Yihe, FU Bojie, HU Jian. Hydrological Services by Mountain Ecosystems in Qilian Mountain of China: A Review . Chinese Geographical Science, 2016, 26(2): 174-187. doi: 10.1007/s11769-015-0791-9
[5]	ZHANG Jifei, DENG Wei, LIU Shaoquan. Geographical Space Development Zone Classification:An Essential Guide for Transformation of Mountain Resource Cities . Chinese Geographical Science, 2015, 25(3): 361-374. doi: 10.1007/s11769-015-0755-0
[6]	ZHANG Yubin, CAO Ning, XU Xiaohong, ZHANG Feng, YAN Fei, ZHANG Xinsheng, TANG Xinlong. Relationship Between Soil and Water Conservation Practices and Soil Conditions in Low Mountain and Hilly Region of Northeast China . Chinese Geographical Science, 2014, 0(2): 147-162. doi: 10.1007/s11769-013-0620-y
[7]	ZHANG Haiyan, QIAN Yibing, WU Zhaoning, WANG Zhongchen. Vegetation-environment Relationships Between Northern Slope of Karlik Mountain and Naomaohu Basin, East Tianshan Mountains . Chinese Geographical Science, 2012, 22(3): 288-301.
[8]	YANG Zhao, LU Lin. Analysis of Social Integration Models of Tourism Labor Migrants——A Case Study of Jiuhua Mountain of Anhui Province, China . Chinese Geographical Science, 2008, 18(2): 127-136. doi: 10.1007/s11769-008-0127-0
[9]	SU Qin, CAO You-hui, LIN Bing-yao. COMPARATIVE STUDY ON RESIDENTS' PERCEPTION OF TOURISM IMPACT AT TOURIST PLACES-A Case Study of Xidi, Zhouzhuang and Jiuhua Mountain . Chinese Geographical Science, 2005, 15(1): 70-79.
[10]	YANG Xiao-zhong, LU Lin, ZHANG Guang-sheng, LU Song, XUAN Guo-fu. RELATIONSHIP BETWEEN RESORT LIFE CYCLE AND RESIDENTS' PERCEPTION AND ATTITUDE——A Case Study of Putuo Mountain . Chinese Geographical Science, 2004, 14(1): 90-96.
[11]	WANG De-gen. PUSH-PULL FACTORS IN MOUNTAIN RESORTS——A Case Study of Huangshan Mountain as World Heritage . Chinese Geographical Science, 2004, 14(4): 368-376.
[12]	WANG Qing, LI Hui-xia, CHEN Guo-jie, CHEN Yong. ANALYSIS ON POVERTY IN MOUNTAIN AREAS BASED ON OFF-FARM INDUSTRIES . Chinese Geographical Science, 2003, 13(4): 359-363.
[13]	ZANG Shu-ying, YUAN Hui, NING Jing. THE LANDSCAPE ECOLOGICAL ASSESSMENT AND PLANNING IN THE CONTROL WATERSHED BY RESERVOIR OF ERLONG MOUNTAIN . Chinese Geographical Science, 2002, 12(2): 176-181.
[14]	HOU Wei-ling, FAN Hong. ECOLOGICAL SERIES OF SOIL ANIMALS IN DARLIDAI MOUNTAIN . Chinese Geographical Science, 2002, 12(4): 378-382.
[15]	ZHANG Hui-yuan, ZHAO Xin-yi, CAI Yun-long, LIU Song. HUMAN DRIVING MECHANISM OF REGIONAL LAND USE CHANGE:A CASE STUDY OF KARST MOUNTAIN AREAS OF SOUTHWESTERN CHINA . Chinese Geographical Science, 2000, 10(4): 289-295.
[16]	KANG Shi-chang, QIN Da-he, YAO Tan-dong, PAUL A. Mayewski, SALLIE Whitlow. FRESH SNOW CHEMISTRY FROM HIGH MOUNTAIN REGIONS IN CENTRAL HIMALAYAS . Chinese Geographical Science, 2000, 10(3): 218-225.
[17]	王直军, Chris Carpenter. FOREST LANDSCAPE AND BIRD DIVERSITY IN MOUNTAIN REGION, XISHUANGBANNA, YUNNAN . Chinese Geographical Science, 1999, 9(2): 172-176.
[18]	祝功武, 刘瑞华. CULTIVATED LAND RESOURCES AND ITS DEVELOPMENT IN THE TROPIC AND SUBTROPIC MOUNTAIN AREAS OF SOUTH CHINA ——A Case Study in Deqing County . Chinese Geographical Science, 1998, 8(4): 362-369.
[19]	甘健民, 薛敬意, 赵恒康. CHANGE OF NUTRIENT IMPORT AND EXPORT IN PROCESS OF RAINFALL IN AILAO MOUNTAIN OF YUNNAN PROVINCE . Chinese Geographical Science, 1996, 6(2): 155-165.
[20]	刘志群, 王荣英. MODEL OF AGRICULTURAL ECOLOGIC-ECONOMIC SYSTEM IN THE INTERMONTANE BASINS OF XUEFENG MOUNTAIN REGION . Chinese Geographical Science, 1993, 3(1): 61-73.

点击查看大图

计量

文章访问数: 790
HTML全文浏览量: 30
PDF下载量: 949
被引次数: 0

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

收稿日期: 1997-01-20

刊出日期: 1997-09-20

关键词:

Lushan Mountain /

Huangshan Mountain /

Tianmu Mountain /

Quaternary deposit environment

摘要: The data of Fe³⁺/Fe²⁺ show that the lowest annual air temperature of the Lushan,Huangshan and Tianmu mountains was not below 0℃, therefore, glacier couldn't develop in there regions. According to palaeomagnetic test combined with the phenomenon of reticulate pattern ground and lithologic identification, the authors elaborate that the “Poyang moraine” is mainly the fluvial sediments of the early period of the Middle Pleistocene. It was formed by transposition of the ancient Ganjiang River under the humid hot climate. For CM image, the Dajiaochang profile of the Lushan Mountain is very similar to periglacial and the debris flow deposits, but the profile of Jiangpochang and Yaoshaling have many kinds of geneses, i.e., debris flow, water debris flow and alluvial etc. In the south piedmont of the Huangshan Mountain, slope gravity and slope seasonal running water transportantion are mainly deposit factors. In the “glacial varve” of the Denglongqiao profile of the Tianmu Mountain, its CaO and Na₂O content is lower than the nonglacial varve, the fact shows that it has the features of the violent leaching, weathering and nonglacial action.

留言板

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

计量

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

English Abstract

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

全文HTML

目录

留言板

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

计量

出版历程

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

English Abstract

COMPARISON OF QUATERNARY DEPOSIT ENVIRONMENT AMONG LUSHAN,HUANGSHAN AND TIANMU MOUNTAINS

Department of City and Resources Sciences, Nanjing University, Nanjing 210093, P. R. China

全文HTML

目录