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黔北后槽下石炭统含铝岩系的粘土矿物
引用本文:杨光龙,朱德彬,王林,潘家州.黔北后槽下石炭统含铝岩系的粘土矿物[J].华南地质与矿产,2008(4):8-13.
作者姓名:杨光龙  朱德彬  王林  潘家州
作者单位:1. 贵州省地质矿产勘查开发局106地质大队,贵州,遵义,563000;中国地质大学,武汉,430074
2. 贵州省地质矿产勘查开发局106地质大队,贵州,遵义,563000
摘    要:为揭示黔北下石炭统含铝岩系的沉积环境,本文利用贵州遵义县后槽TC718剖面系统试样的粘土矿物进行x一射线衍射测试及特征分析。含铝岩系粘土岩与下伏桐梓组粘土页岩在矿物组合和成分上均有明显的差异,水云母的结晶度指数、开形指数在剖面纵向上有三个变化拐点:一是含铝岩系与下伏桐梓组粘土页岩分界处;二是含铝岩系上、下段的接触带;三是含铝岩系顶部含炭质粘土岩出现的临界面。其变化特征表明,本区下石炭统含铝岩系粘土岩段为海相或海陆过渡相,铝质岩段为残积一坡积相,顶部为大陆湖沼相;下奥陶统桐梓组页岩段为海相。

关 键 词:X-射线衍射分析  粘土矿物  含铝岩系  沉积环境  遵义县  贵州

Clay Minerals in Aluminiferous Rock System of Lower Carboniferous in Houcao,North Guizhou
YANG Guang-long,ZHU De-bin,WANG Lin,PAN Jia-zhou.Clay Minerals in Aluminiferous Rock System of Lower Carboniferous in Houcao,North Guizhou[J].Geology and Mineral Resources of South China,2008(4):8-13.
Authors:YANG Guang-long  ZHU De-bin  WANG Lin  PAN Jia-zhou
Institution:YANG Guang-long1,2,ZHU De-bin1,WANG Lin1,PAN Jia-zhou1(1.No.106 Geological Brigade,Guizhou Bureau of Geology , Minerals Exploration & Development,Zunyi 563000,Guizhou,China,2.China University of Geosciences,Wuhan 430074,Hubei,China)
Abstract:In order to reveal the sedimentary environment around aluminiferous rock system of lower Carboniferous,this paper takes clay minerals of the Houcao TC718 profile in Zunyi County,Guizhou as the sample for X-ray diffraction test and the characteristics analysis.Clay rocks of aluminiferous rock system are obviously different from clay shale of underlying Tungtzu group in the mineral compounding and component.There are three changes in inflexion of the crystallization index,the open form index of hydromica in v...
Keywords:X-ray diffraction analysis  Clay mineral  Aluminiferous rock system  Sedimentary environment  Zunyi County  Guizhou  
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