引用本文:龚黎明,王长生.渝东南秀山酉阳地区南华系沉积环境初步研究(J/M/D/N,J:杂志,M:书,D:论文,N:报纸).期刊名称,2012,29(9):70-75
CHEN X. Adap tive slidingmode contr ol for discrete2ti me multi2inputmulti2 out put systems[ J ]. Aut omatica, 2006, 42(6): 4272-435
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渝东南秀山酉阳地区南华系沉积环境初步研究
龚黎明,王长生
作者单位
龚黎明,王长生  
摘要:
在重庆市东南部,南华系只分布在秀山县和酉阳县,可细分为3个组:南沱组、大塘坡组和千子门组。其中南沱组和千子门组为冰碛层,沉积环境为低碛层、冰内河道相、冰前冰河相、冰前海湾泻湖相和冰前滨海相;大塘坡组为海湾泻湖相沉积,形成了大型锰矿床。区内南华纪气候具备典型的三段式结构特征:上、下两个冰期,中间夹一个间冰期,亦即南沱期、大塘坡间冰期和千子门期。
关键词:  秀山酉阳地区  南华系  冰碛层
DOI:
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Preliminary Study on Sedimentary Environment of the Nanhuan System of Xiushan and Youyang Area in Southeast Chongqing
GONG Li-ming,WANG Chang-sheng
Abstract:
In southeast Chongqing City,the Nanhuan System is only found in Xiushan and Youyang County and can be divided into three Formations:Nantuo Formations,Datangpo Formations and Qianzimen Formations,of which Nantuo Formations and Qianzimen Formations are Drift sheet,and their ssedimentary enviroment is glacial ground moraine-tillite facies,Lensatis sand-condlomerate facies in englacial channel,proglacial littora facies,forming a large managanese deposit,Nanhuan Period climate has the typical three-stage structural features:the upper and lower glacial,sandwhiched between an interglacial,i.e.Natuo glacia stage,the interglacial of Datangpo and Qianzimen glacial.
Key words:  Xiushan and Youyang area  Nanhuan System  Drift sheet  sedimentary facies  Nantuo Formations  Datangpo Formations  Qianzimen Formations
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