[1]刘 丹,等.江西南城醉仙湖河口组地层沉积特征及景观成因分析[J].山地学报,2018,(02):239-247.[doi:10.16089/j.cnki.1008-2786.000319]
　LIU Dan,LUO Yong,et al.Strata Sedimentary Characteristics and Landscape Genetic Analysis of the Hekou Formation at the Zuixian Lake, Nancheng, Jiangxi Province, China[J].Mountain Research,2018,(02):239-247.[doi:10.16089/j.cnki.1008-2786.000319]
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江西南城醉仙湖河口组地层沉积特征及景观成因分析()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2018年02期
页码:
239-247
栏目:
山地环境
出版日期:
2018-03-30

文章信息/Info

Title:
Strata Sedimentary Characteristics and Landscape Genetic Analysis of the Hekou Formation at the Zuixian Lake, Nancheng, Jiangxi Province, China
文章编号:
1008-2786-(2018)2-239-09
作者:
刘 丹1;  2;  罗 勇2*; 杨庆坤1;  2; 黄宝华2; 曲宏健2
1.东华理工大学 放射性地质与勘探技术国防重点学科实验室,南昌 330013; 2.东华理工大学 地球科学学院, 南昌330013
Author(s):
LIU Dan1;  2;  LUO Yong2; YANG Qingkun1;  2; HUANG Baohua2; QU Hongjian2
1.Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China University of Technology, Nanchang 330013, China; 2.School of Earth Sciences, East China University of Technology, Nanchang 330013, China
关键词:
醉仙湖;  丹霞地貌;  白垩系;  辫状河相沉积
Keywords:
Zuixian Lake;  Danxia;  cretaceous;  braided river sediments
分类号:
K92
DOI:
10.16089/j.cnki.1008-2786.000319
文献标志码:
A
摘要:
江西南城东南部地区广泛发育上白垩统河口组巨厚红层,丹霞丘陵地貌被翠绿的湖水分割为众多岛屿,形成了“绿水绕红山”的独特景象,是醉仙湖景区的主要地貌景观。关于丹霞地貌景观的成因机制,不同区域往往主控因素也不一致。为了增强地质公园建设过程中的科普价值,就需要对红层成岩-成景过程中的地质作用有着详细的了解。本文按控制红盆成景的主导动力因素,将研究区醉仙湖内发育的丹霞地貌详细划分为丹霞构造地貌、丹霞水蚀地貌、丹霞风蚀地貌、丹霞盐风化地貌等多种类型。通过对研究区红层的岩石学特征、沉积相带划分以及景观地貌特征等因素的分析,笔者认为研究区成景地层主要为一套白垩系红层辫状河相砂砾岩,为丹霞地貌的形成奠定了物质基础,成岩期后的内外动力作用对景观成因有着重要的约束作用。
Abstract:
The thick redbed of the upper cretaceous Hekou Formation is widely distributed over the southwest of Nancheng, Jiangxi Province, forming Danxia hilly landforms.The Danxia hilly landscapes have shaped into islands surrounded by green lake water, forming a unique scene of “green water around red cliff” which is the main tourism attraction of the Zuixian Lake Scenic Area.According to types of geological driving forces, the Danxia landforms developed in the Zuixian Lake were assorted into various types, such as Danxia tectonic landform, Danxia water erosion landform, Danxia wind erosion landform, and Danxia salt weathered landform.Through field investigations and indoor analysis, the deposition feature of the braided river facies of the cretaceous redbed in the study area was systematically analyzed.From the geological point of view, the sedimentary characteristics, internal and external dynamic geologic actions of the cretaceous redbed were expounded in detail respectively.Results suggested that the lithofacies in the area lay the material foundation for the formation of the Danxia landscape, and its sedimentary types, internal and external geologic dynamics play an important role in constraining the landscape development.

参考文献/References:

[1] 彭华.中国丹霞地貌研究进展[J].地理科学, 2000, 20(3):203-211[PENG Hua.A survey of the Danxia Landform Research in China[J].Scientia Geographica Sinica, 2000, 20(3):203-211.]
[2] 朱志军, 黄宝华, 郭福生等.龙虎山世界地质公园白垩系辫状河相沉积及其丹霞地貌发育特征[J].地球学报, 2012,33(2): 1-9[ZHU Zhijun, HUANG Baohua, GUO Fusheng, et al.Cretaceous braided river facies sediments and Danxia landform development characteristics in Longhushan world geopark, Jiangxi [J].Act Geoscientica Sinica, 2012,33(2): 1-9.]
[3] 曾昭璇, 黄少敏.中国东南部红层地貌[J].华南师院学报(自然科学版), 1978,(1):56-73 [ZENG Zhaoxuan, HUANG Shaomin.Red beds landform in Southeast China[J].Journal of South China Normal University(Natural Science), 1978,(1):56-73]
[4] 郭福生,刘林清,杨志等.江西省丹霞地貌发育规律及旅游区域研究[J].资源调查与环境,2007,28(3),214-222.[GUO Fusheng, LIU Linqing, Yang Zhi, et al.Development of Danxia landform in Jiangxi province and its regional planning for tourism[J].Resources Survey & Environment,2007,28(3),214-222.]
[5] 黄进, 陈致均.丹霞地貌定义及分类中一些问题的探讨[J].经济地理, 2003,23(增刊):6-11.[HUANG Jin, CHEN Zhijun.The discussion on the definition and classification to Danxia landform[J].Economic Geography, 2003,23(supp):6-11.]
[6] 赵逊, 赵汀.地质公园发展与管理[J].地球学报, 2009, 30(3):301-308.[ZHAO Xun, ZHAO Ting.Development and management of geopark[J].Acta Geoscientica Sinica, 2009, 30(3):301-308.]
[7] 郭福生, 姜勇彪, 胡中华等.龙虎山世界地质公园丹霞地貌成景系统特征及其演化[J].山地学报,2011,29(2): 195-201.[GUO Fusheng, JIANG Yongbiao, HU Zhonghua,et al.Evolution and Genesis System Features of Danxia Lanform in Longhushan World Geopark[J].Mountain Research,2011,29(2): 195-201.]
[8] 姜勇彪, 郭福生, 刘林清等.江西信江盆地丹霞地貌形成机制分析[J].热带地理, 2011, 31(2):146-152.[JIANG Yongbiao, Guo Fusheng, LIU Linqing, et al.A study on Genesis of Danxia landforms in the Xinjiang Basin,Jiangxi[J].Tropical Geography, 2011, 31(2):146-152.]
[9] 姜勇彪, 郭福生, 陈珊珊.江西信江盆地丹霞地貌空间分布及其成因[J].山地学报, 2013, 31(6): 731-737.[JIANG Yongbiao,GUO Fusheng,CHEN Shanshan.Spatial Distribution and Its Genesis of the Danxia Landforms in Xinjiang Basin,Jiangxi[J].Mountain Research, 2013, 31(6): 731-737.]
[10] 彭华.丹霞地貌分类系统研究[J].经济地理, 2002,22(S1): 28-35[PENG Hua.The Research on classification system of Danxia landform[J].Economic Geography, 2002,22(S1): 28-35]
[11] ZHU C, PENG H, OU Y et al.Rock resistance and the development of horizontal grooves on Danxia slopes[J].Geomorphology, 2010,123(1-2):84-96.
[12] 马春梅,朱诚,彭华.安徽齐云山丹霞地貌成因[J].地理学报:英文版.2006,16(1):45-56.[MA Chunmei, ZHU Cheng, PENG Hua, et al.Danxia landform genesis of the Qiyun Mountain, Anhui Province[J].Geomorphology,2006,16(1):45-56.]
[13] QI D, YU R, ZHANG R, et al.Comparative studies of Danxia landforms in China[J].Journal of geographical sciences,2005,15(3):337-345.
[14] PENG H.Danxia geomorphology of China: A review[J].Chinese Science Bulletin.2001,46(1):38-44.
[15] 陈致均, 黄可光, 戴文昭.甘肃丹霞地貌的分布[J].经济地理, 1994,14(S1): 159-166.[CHEN Zhijun, HUANG Keguang,DAI Wenzhao.Distribution of Danxia landform in Gansu(in English)[J].Economic Geography, 1994,14(S1): 159-166.]
[16] 黄进, 陈致均, 黄可光.丹霞地貌的定义及分类[J].经济地理, 1992,12(增刊):37-49.[HUANG Jin,CHEN Zhijun,HUANG Keguang.Definition and classification of Danxia landform(in English)[J].Economic Geography, 1992,12(supp):37-49.]
[17] 罗成德.四川盆地丹霞地貌旅游资源[J].经济地理, 1996,(S1):170-176 [.LUO Chengde.Tourism resources of Danxia landform in Sichuan Basin(in English)[J].Economic Geography, 1996,(S1):170-176.]
[18] 邓美成, 王光明.崀山丹霞地貌风景的分析与评价[J].经济地理, 1996, 16(S1): 4-20.[DENG Meicheng,WANG Guangming.Analysis and evaluation of Danxia landscape of Lang Mountain(in English)[J].Economic Geography,1996, 16(S1): 4-20.]
[19] 姜勇彪, 郭福生, 孙传敏等.江西弋阳县龟峰丹霞地貌景观特征与形成机制[J].山地学报, 2008,26(1): 120-125.[JIANG Yongbiao, GUO Fusheng, SUN Chuanmin, et al.The Features and Origin of the Danxia Landform in Guifeng Scenic Park in Yiyang County, Jiangxi[J].Mountain Research, 2008,26(1): 120-125.]
[20] 李霞, 何庆成, 董颖等.贵州赤水南部地区丹霞地貌类型特征及成因演化分析[J].地球学报, 2013, 34(4):501-508.[LI Xia, HE Qingcheng, DONG Yin, et al.An Analysis of Characteristics and Evolution of Danxia Landform in the South of Chishui County, Guizhou[J].Acta Geoscientica Sinica, 2013, 34(4):501-508.]
[21] ZHU C, Li W, TONG X et al.Experimental studies on the Danxia landscape morphogenesis in Mt.Danxiashan, South China[J].Journal of Geographical Sciences, 2015,25(8):943-966.
[22] 舒良树.华南构造演化的基本特征[J].地质通报, 2012,31(7):1035-1053.[SHU Liangshu.An analysis of principal features of tectonic evolution in South China Block[J].Geological Bulletin of China,2012,31(7):1035-1053.]
[23] WANG D Z, SHU L S.Late Mesozoic basin and range tectonics and related magmatism in Southeast China.Geoscience Frontier[J].2012, 3(2): 109-124.
[24] 黄进.崀山丹霞地貌[M].北京:科学出版社,2011.[HUANG Jin.Danxia landform of Langshan Mountain[M].Beijing: The Science Publishing Company, 2011.]
[25] 吕洪波, 苏德辰, 章雨旭, 等.中国不同气候带盐风化作用的地貌特征[J].地质论评,2017, 63(4):91-1926.[LV Hongbo, SU Dechen, ZHANG Yuxu, et al.Landform features of salt weathering in different climatic zones in Chian.Geoligical Review[J].2017, 63(4): 911-926.]

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备注/Memo

备注/Memo:
收稿日期(Received date):2016-04-14; 改回日期(Accepted date): 2018-01-25
基金项目(Foundation item):东华理工大学地质资源经济与管理研究中心开放基金项目(14JC03); 国家自然科学基金项目(41772197; 41602069); 江西省自然科学基金项目(20171BAB213026); 东华理工大学地质资源经济与管理研究中心开放基金项目(14JC01)。[Geological Resource Economics and Management Research Center Open Fund of East China University of Technology(14JC03); National Natural Science Foundation of China(41772197; 41602069); Natural Science Foundation of Jiangxi,China(20171BAB213026); Geological Resource Economics and Management Research Center Open Fund of East China University of Technology(14JC01).]
作者简介(Biography):刘丹(1986-),女,陕西西安人,硕士研究生,主要研究方向:地貌第四纪及人文地理。[LIU Dan(1986-), Female, born in Xi'an, Shanxi province, M.Sc.candidate, research on human geography and geomorphology quaternary.] E-mail: 459520795@qq.com.
*通讯作者(Corresponding author):罗勇(1982-),男,硕士,讲师,主要研究方向:区域地质及旅游地学。 [LUO Yong(1982-), male, M.Sc., lecturer, specialized in regional geology and tourism geoscience.] E-mail: 522833533@qq.com.
更新日期/Last Update: 2018-03-30