|本期目录/Table of Contents|

[1]林春明,张妮,张霞,等.安徽巢湖平顶山西坡剖面下三叠统殷坑组瘤状灰岩特征[J].地球科学与环境学报,2017,39(04):476-490.
 LIN Chun-ming,ZHANG Ni,ZHANG Xia,et al.Characteristics of Nodular Limestone from the Lower Triassic Yinkeng Formation at West Pingdingshan Section in Chaohu of Anhui, China[J].Journal of Earth Sciences and Environment,2017,39(04):476-490.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第39卷
期数:
2017年第04期
页码:
476-490
栏目:
基础地质与矿产地质
出版日期:
2017-07-28

文章信息/Info

Title:
Characteristics of Nodular Limestone from the Lower Triassic Yinkeng Formation at West Pingdingshan Section in Chaohu of Anhui, China
文章编号:
1672-6561(2017)04-0476-15
作者:
林春明张妮张霞于进王淑君
1.南京大学 内生金属矿床成矿机制研究国家重点实验室,江苏 南京 210046; 2.南京大学 地球科学与工程学院,江苏 南京 210046; 3.金陵科技学院 材料工程学院,江苏 南京 211169
Author(s):
LIN Chun-ming ZHANG Ni ZHANG Xia YU Jin WANG Shu-jun
1. State Kay Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210046, Jiangsu, China; 2. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210046, Jiangsu, China; 3. School of Materials Engineering, Jinling Institute of Technology, Nanjing 211169, Jiangsu, China
关键词:
沉积特征沉积环境瘤状灰岩矿物组成地球化学殷坑组下三叠统安徽
Keywords:
sedimentary characteristic sedimentary environment nodular limestone mineral composition geochemistry Yinkeng Formation Lower Triassic Anhui
分类号:
P184
DOI:
-
文献标志码:
A
摘要:
对安徽巢湖平顶山西坡剖面下三叠统殷坑组瘤状灰岩中瘤体与基质的矿物组成、结构、构造、化学成分及地球化学等进行了系统研究。结果表明:瘤状灰岩在殷坑组极其发育,由瘤体和基质两部分组成;瘤体主要多为灰色、浅灰色或灰白色微晶灰岩、泥晶微晶灰岩和微晶泥晶灰岩,主要矿物是方解石,占整个瘤体的54%~85%,次为石英、斜长石和黏土矿物等陆源物质,还含少量的黄铁矿;基质颜色较深,以黄色、褐黄色和黄灰色钙质泥岩为主,泥质微晶灰岩次之,与瘤体相比,基质中方解石矿物明显减少,石英、黏土矿物明显增加,斜长石含量变化不大;按瘤体的排列方式将瘤状灰岩划分为断续状、条带状和杂乱状3种类型,其是后期差异性压实与压溶作用逐渐增强的结果;剖面中断续状瘤状灰岩最先出现,而且出现的层位多,厚度大,主要发育在上斜坡环境,仅少量出现在下斜坡,然后为条带状瘤状灰岩,分布在下斜坡,杂乱状瘤状灰岩出现的层位最少,厚度最小,最不发育,仅分布在深水盆地环境。
Abstract:
The mineral composition, structure, chemical composition and geochemistry characteristics of nodules and matrix from Lower Triassic Yinkeng Formation at West Pingdingshan section in Chaohu of Anhui, China were systematically studied. The results show that nodular limestones are composed of nodules and matrix, and develop well in Yinkeng Formation; nodules are mainly composed of microcrystalline limestone, micritic micrite and microcrystalline micrite calcite with the color dominated by gray, light gray and gray white; the main minerals of nodules are mainly calcite, accounts for 54%-85%, the rest part is made up of quartz, plagioclase and clay minerals, and also contain a small amount of pyrite; the matrix occurs predominantly of yellow, brown-yellow and yellow-gray calcareous mudstones, followed with pelmicrite; compared to nodules, matrix contains less calcite mineral, more quartz and clay minerals; there are three types of the nodular limestone, including banded nodular limestone, discontinuous nodular limestone and random nodular limestone; the three types are the result of combined processes of the differential compaction, and gradually enhance pressure solution during the diagenesis; discontinuous nodular limestone occurs first within many layers and thicker, and develops mainly in the upper part of slope; then, banded nodular limestone distributes in the lower part of slope; at last, random nodular limestone is thinner and develops poor, only appears in deep water basin environment.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2017-02-16
基金项目:国家自然科学基金项目(41272124)
作者简介:林春明(1964-),男,福建龙海人,教授,博士研究生导师,理学博士,博士后,E-mail:cmlin@nju.edu.cn。
更新日期/Last Update: 2017-07-28