[1]张信宝.运用地貌垂直地带性理论判别庐山第四纪冰川有无[J].山地学报,2016,(02):129-133.[doi:10.16089/j.cnki.1008-2786.000109]
 ZHANG Xinbao.Discrimination of Quaternary Glaciation in the Lushan Mountain of East China by Using Vertical Geomorphology Zone Theory[J].Mountain Research,2016,(02):129-133.[doi:10.16089/j.cnki.1008-2786.000109]
点击复制

运用地貌垂直地带性理论判别庐山第四纪冰川有无()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年02期
页码:
129-133
栏目:
专家观点
出版日期:
2016-04-01

文章信息/Info

Title:
Discrimination of Quaternary Glaciation in the Lushan Mountain of East China by Using Vertical Geomorphology Zone Theory
作者:
张信宝
中国科学院水利部成都山地灾害与环境研究所,四川 成都 610041
Author(s):
ZHANG Xinbao
Institute of Mountain Hazards and Environment, CAS,Chengdu 610014,China
关键词:
地貌垂直地带性 岩性 赣北庐山 浙西千里岗山 第四纪冰川
Keywords:
vertical geomorphology zone lithology Lushan Mountain in North Jiangxi Qianligang Mountain in West Zhejiang Quaternary glaciation
分类号:
P931
DOI:
10.16089/j.cnki.1008-2786.000109
文献标志码:
A
摘要:
庐山东约300 km的浙西千里岗山,海拔1 523 m,高于庐山1 474 m,山顶出露岩层为夹粉砂质泥岩的岩屑石英砂岩的志留系上统唐家坞组,岩性软弱。以赣北庐山为代表的中国东部第四纪冰川问题,是我国地质、地理学界争议最大、认识最分歧的重大问题,“庐山第四纪冰川”认识分歧的重要原因是山地侵蚀地貌形态和相应堆积物的多解性。依据地貌垂直地带性理论,软弱岩层的分布高程,不可能超过冰川地貌带上限,也就是说,没有达到冰川地貌带的高度。为此,通过 “跳出庐山看庐山”,判别庐山第四纪冰川的有无。认为,千里岗山与包括庐山在内的邻近地区的同高程山地的高度无第四纪冰川发育。
Abstract:
Quaternary glaciation in the low mountain-hill regions of East China, represented by Lushan Mountain in North Jiangxi, is one of the most controversy and divergent issues in geology and geography in China, because of multiple explanations of the erosive landforms and the relative deposits. The issue on the quaternary glaciation in the Lushan Mountain is discriminated by using a way of “Out of Mount Lu to see Mount Lu”. Qianligang Mountain in West Zhejiang, 300 km east to the Lusha Mountain, has an elevation of 1 523 m, which is higher than 1 474 m of the later. Clastic rocks of the Tangjiawu Group of Upper Silurian, such as sandstone, siltstone and mudstones are outcropped at the peak of Qianligang Mountain. According to vertical geomorphology zone theory, the highest distribution elevation of those types of soft rocks is limited to the upper elevation of the perglacial zone,in other words, don't reach to the elevation of the glacial zone. Therefore, Qianligang Mountain and the other mountains with similar or less elevations including Lushan Mountain have no glaciations.

参考文献/References:

[1] 李四光.冰期之庐山[M].前中央研究院地质研究所乙种,第二号,1947.[Li Siguang. Quaternary Glaciations in Lushan Area, Central Cjina[M].Academia Sinica, Monography of the Institute of Geology, Series B,Ⅱ,Nanking. 1947.]
[2] 孙殿卿,杨怀仁.大冰期时期中国的冰川遗迹[J].地质学报,1961,41(3/4):233-244[Sun Dianqing,Yang Huairen. Glacial relics in China during the period of the great ice age[J]. Journal of Geology, 1961,41(3/4):233-244]
[3] 孙殿卿, 何培元. 近20 年来中国第四纪冰川研究的进展[J]. 地球科学-中国地质大学学报, 1994, 19(6): 838-844[Sun Dianqing, He Peiyuan. On advancement in study of Quaternary Glaciation in recent 20 years [J]. Earth Science Journal of China University of Geosciences, 1994, 19(6): 838-844]
[4] 任美锷. 庐山地形的初步研究[J].地理学报,1953,19(1):61-73[Ren Meie. Preliminary study on the terrain of Mount Lu[J].Journal of Geography, 1953,19(1):61-73]
[5] 施雅风. 庐山真的有第四纪冰川吗?[J].自然辩证法通讯,1981,2:41-45[Shi Yafeng. Does Mount Lu really have Quaternary glaciers? [J]Journal of Dialectics of Nature, 1981,2:41-45]
[6] 徐馨, 沈志达, 何才华. 对长江中下游第四纪冰川发育的新认识[J ]. 贵州师范大学学报:自然科学版,1999, 17(1):1- 6[Xu Xin, Shen Zhida, He Caihua. A new idea to Quaternary Glaciation in the middle and lower reaches of the Changjiang River[J ]. Journal of Guizhou Normal University:Natural Science, 1999, 17(1):1-6]
[7] 黄培华. 关于长江以南地区第四纪冰川遗迹问题[J].科学通报,1963,10:29-33[Huang Peihua. Problems on whether the quaternary glacial remains in the south of the Yangtze River[J]. Science Bulletin, 1963,10:29-33]
[8] 周廷儒.近30年中国第四纪古地理研究的进展[J].地理学报,1979,4:279-292[Zhou Tingru. Progress of Quaternary ancient geography in China in recent 30 years[J].Journal of Geography, 1979,4:279-292]
[9] 任美锷,刘泽纯,王富葆.对庐山第四纪冰川问题的几点意见[J].自然辩证法通讯,1982,2:37-39[Ren Meie, Liu Zechun, Wang Fubao. Several opinions on the Quaternary glacier in Mount Lu[J].Journal of Dialectics of Nature, 1982,2: 37-39]
[10] 施雅风, 李吉均. 80 年代以来中国冰川学和第四纪冰川研究的新进展[J ]. 冰川冻土, 1994, 16(1):1-14[Shi Yafeng, Li Jijun. New progress on the glaciological and Quaternary Glaciation research in China since the 1980s [J].Journal of Glaciology and Geocryology, 1994, 16(1):1-14]
[11] 李吉均, 舒强, 周尚哲, 等. 中国第四纪冰川研究的回顾与展望[J]. 冰川冻土, 2004, 26(3):235-243[Li Jijun, Shu Qiang, Zhou Shangzhe, et al. Review and prospects of Quaternary Glaciation research in China [J]. Journal of Glaciology and Geocryology, 2004, 26(3):235-243]
[12] Derbyshire,E. A History of Glacial Stratigraphy in China[J].Quaternary Science Reviews,1987,6:301-314
[13] 张信宝,周立平,汪阳春,等.地带性与非地带性夷平面[J].第四纪研究,2007,27(1):93-99[Zhang Xinbao, Zhou Liping, Wang Yangchun, et al. Zonal and non-zonal planation surfaces[J].Quaternary Sciences, 2007,27(1):93-99]
[14] 张信宝,吴积善,汪阳春,等.川西北高原的地貌垂直地带性与寒冻夷平面[J].山地学报,2006,24(5):607-611[The vertical zone and the cold frozen zone in the Northwest Sichuan Plateau[J]. Mountain Research,2006,24(5):607-611]
[15] Zhang Xinbao, He Xiubin, Wang Yangchun,et al.Planation surfaces on the Tibet Plateau, China[J].Journal of Mountain Sciences,2008(5):310-317
[16] 夏正楷. 太白山古冰川地貌与地质构造[J]. 冰川冻土, 1990,12(2):155-160[Xia Zhengkai, The ancient glacial relief and faulting tectonies in the Taibaishan Qinling Mts[J].Journal of Glaciology and Geocryology, 1990, 12(2):155-160]
[17] 肖荣寰,胡俭彬.东北地区末次冰期以来气候地貌的若干特征 [J]. 冰川冻土, 1988, 10(2):125-134[Xiao Ronghuan, Hu Junbin.Some characteristics of the climatic landform in the Northeast China since the glacial Epoch[J]. Journal of Glaciology and Geocryology,1988, 10(2):125-134]
[18] Cui Zhijiu, Yang Jianfu, Liu Gengnian, et al. Discovery of Quaternary glacial evidence of Snow Mountain in Taiwan, China [J]. Chinese Science Bullentin,2000,45(6):565-571
[19] 中华人民共和国地质矿产部,地质专报,一 区域地质,第十一号,浙江省区域地质志[M].北京:地质出版社,1989:688[Ministry of Geology and Mineral Resources of the People's Republic of China. Geological special report, one regional geology, the eleventh, Regional geology of Zhejiang Province[M].Beijing:Geological Press, 1989:688]

相似文献/References:

[1]张信宝,吴积善,汪阳春,等.川西北高原的地貌垂直地带性与寒冻夷平面[J].山地学报,2006,(05):607.
[2]张信宝,刘维明,陈宁生,等.青藏高原面地貌稳定态与高原隆升时间[J].山地学报,2023,(4):459.[doi:10.16089/j.cnki.1008-2786.000762 ]
 ZHANG Xinbao,LIU Weiming,CHEN Ningsheng,et al.Geomorphological Steady State of the Tibet Plateau and Its Uplift Time[J].Mountain Research,2023,(02):459.[doi:10.16089/j.cnki.1008-2786.000762 ]

备注/Memo

备注/Memo:
收稿日期(Received date):2015-10-11; 改回日期(Accepted): 2015-10-19。 作者简介(Biography):张信宝(1946-),男,江苏镇江人,博士生导师,现从事地质地貌研究。[Zhang Xinbao(1946-),male, was born in Zhenjiang, Jiangsu province, professor, mainly engaged in research of geomorphology.] E-mail:zxbao@imde.ac.cn
更新日期/Last Update: 1900-01-01