[an error occurred while processing this directive] 世界地质 2020, 39(3) 578-589 DOI:   10.3969/j.issn.1004-5589.2020.03.007  ISSN: 1004-5589 CN: 22-1111/P

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兴城地区
常州沟组
沉积物源
构造背景
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修铭
高福红
贾啸宇
龚辉
PubMed
Article by Xiu M
Article by Gao F
Article by Jia X
Article by Gong H
兴城地区常州沟组沉积物源及其构造背景分析
修铭, 高福红, 贾啸宇, 龚辉
吉林大学地球科学学院, 长春 130061
摘要: 笔者在常州沟组岩石样品岩石学特征研究的基础上,利用碎屑组分分析和地球化学数据分析等方法,探究兴城地区常州沟组地层沉积物源特征及其构造背景。研究表明,研究区常州沟组岩石样品物源多来自于相对成熟的酸性岩石,以沉积岩和花岗岩为主,经历中等偏弱的风化作用,其源区构造背景相对比较稳定,可能为被动大陆边缘。
关键词 兴城地区   常州沟组   沉积物源   构造背景  
Analysis of sediment provenance and tectonic background of Changzhougou Formation in Xingcheng area
XIU Ming, GAO Fu-hong, JIA Xiao-yu, GONG Hui
College of Earth Sciences, Jilin University, Changchun 130061, China
Abstract: Based on the petrological study of rock samples from Changzhougou Formation, the methods of clastic composition analysis and geochemical data analysis are used to explore the sedimentary source characteristics and tectonic background of Changzhougou Formation in Xingcheng area. The results show that the provenance of the Changzhougou Formation in the study area is mainly relatively mature acid rocks, including sedimentary rocks and granites, which experienced moderate to weak weathering. The tectonic background of the provenance area is relatively stable, and the tectonic setting is likely passive continental margin.
Keywords: Xingcheng area   Changzhougou Formation   sediment provenance   tectonic background  
收稿日期 2020-03-28 修回日期 2020-05-02 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2020.03.007
基金项目:

吉林大学兴城教学基地建设研究项目(PB2014002)资助

通讯作者: 高福红(1963-),女,教授,博士生导师,主要从事岩石学方面研究。E-mail:gaofh@mails.jlu.edu.cn
作者简介:
作者Email: gaofh@mails.jlu.edu.cn

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