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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 被引量:2

Strata Sedimentary Characteristics and Landscape Genetic Analysis of the Hekou Formation at the Zuixian Lake,Nancheng,Jiangxi Province,China
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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。 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 fiver 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 suggested that the lithofacies in the area lay the material foundation for its sedimentary types, internal and external geologic dynamics play an development. expounded in detail respectively. Results the formation of the Danxia landscape, and important role in constraining the landscape
作者 刘丹 罗勇 杨庆坤 黄宝华 曲宏健 LIU Dan;LUO Yong;YANG Qingkun;HUANG Baohua;QU Hongiian(Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China University of Technology Nanchang 330013, China;School of Earth Sciences, East China University of Technology, Nanchang 330013, China)
出处 《山地学报》 CSCD 北大核心 2018年第2期239-247,共9页 Mountain Research
基金 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) 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) 国家自然科学基金项目(41772197 41602069) 江西省自然科学基金项目(20171BAB213026)~~
关键词 醉仙湖 丹霞地貌 白垩系 辫状河相沉积 Zuixian Lake Danxia cretaceous braided river sediments
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