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首页|期刊导航|世界核地质科学|鄂尔多斯盆地伊和乌素地区环河组砂岩地球化学特征及对物源区、构造背景的指示

鄂尔多斯盆地伊和乌素地区环河组砂岩地球化学特征及对物源区、构造背景的指示

罗腾 张字龙 贺锋 张艳

世界核地质科学2024,Vol.41Issue(2):261-274,14.
世界核地质科学2024,Vol.41Issue(2):261-274,14.DOI:10.3969/j.issn.1672-0636.2024.02.004

鄂尔多斯盆地伊和乌素地区环河组砂岩地球化学特征及对物源区、构造背景的指示

Geochemical characteristics of Huanhe formation sandstones in Yihewusu area of Ordos basin and the indications to provenance area and tectonic setting

罗腾 1张字龙 1贺锋 1张艳1

作者信息

  • 1. 核工业北京地质研究院 中核集团铀资源勘查与评价技术重点实验室,北京 100029
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摘要

Abstract

In order to explore the tectonic background and material sources of the sandstones of Lower Cretaceous Huanhe formation,the petrological and geochemical characteristics of the sandstones of Huanhe formation in Yihewusu area of Ordos basin were analyzed mainly through microscopic identification and petrographic and mineralogical tests.The main components of the sandstone of Huanhe formation in Yihewusu area are quartz,feldspar and mica,with small amounts of dark minerals such as pyrite and charcoal fragments.The grains are rounded and sub-angular,poorly sorted,and have the characteristics of near-source deposition.The elemental geochemical analysis on the sandstones are characterized by high SiO2 content(71.69% on average),medium Al2O3 content(12.39%on average)and low content of other elements.The average chemical alteration index(CIA)of the rocks and minerals is 60.92 and the average chemical weathering index(CIW)is 68.47,indicating that the source rocks of the provenance area have experienced moderate intensity weathering.The standardized spider-web diagram of trace element spheroidal meteorites shows that Huanhe formation in the study area enriched in elements such as Ba,Th,La and U,and deficient in elements such as Nb,Zr,Ho and Er.The Rare Earth Element(REE)pattern shows that the sandstones of Huanhe formation in the study area bears negative anomalies in Eu,with an average of 10.23 for LREE/HREE,16.27 for La/Yb,and 11.65 for LaN/YbN.The tectonic background of the sandstones deposition in Yihewusu area was the active continental margin,and the main source area is the felsic igneous rock.It is believed that the original provenance area of the sandstones of Huanhe formation in the Yihewusu area mainly come from the Wolf Mountain and Wulashan diserict.

关键词

砂岩地球化学/构造背景/物源分析/环河组/伊和乌素地区

Key words

sandstone geochemistry/tectonic setting/provenance analysis/Huanhe formation/Yihewusu area

分类

天文与地球科学

引用本文复制引用

罗腾,张字龙,贺锋,张艳..鄂尔多斯盆地伊和乌素地区环河组砂岩地球化学特征及对物源区、构造背景的指示[J].世界核地质科学,2024,41(2):261-274,14.

基金项目

中国铀业地勘项目(编号:202201-8) (编号:202201-8)

中核集团青年英才项目(编号:QNYC2301)和中核集团集中研发项目(编号:中核科发2021-143号)联合资助 Supported by China Nuclear Uranium Geological Exploration Projects(No.202201-8) (编号:QNYC2301)

CNNC Young Genius Projects(No.QNYC2301)and CNNC Centralised Research and Development Projects(No.2021-143) (No.QNYC2301)

世界核地质科学

OACSTPCD

1672-0636

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