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现代地质 ›› 2019, Vol. 33 ›› Issue (02): 284-292.DOI: 10.19657/j.geoscience.1000-8527.2019.02.04

• 矿床学与岩石学 • 上一篇    下一篇

辽宁北部秀水盆地白垩系义县组泥岩地球化学特征及地质意义

李文博(), 李晓海, 丁秋红, 陈树旺, 张健   

  1. 中国地质调查局 沈阳地质调查中心,辽宁 沈阳 110034
  • 收稿日期:2018-08-06 修回日期:2018-11-19 出版日期:2019-05-08 发布日期:2019-05-08
  • 作者简介:李文博,男,工程师,1987年出生,石油地质专业,主要从事油气地质调查工作。Email: 22413816@qq.com
  • 基金资助:
    中国地质调查局项目“松辽外围西部盆地油气基础地质调查”(DD20160163);“松辽盆地北部及外围石炭—二叠系油气地质调查”(DD20190097)

Geochemical Characteristics of the Cretaceous Yixian Formation Mudstones in Xiushui Basin of Northern Liaoning and Their Geological Significance

LI Wenbo(), LI Xiaohai, DING Qiuhong, CHEN Shuwang, ZHANG Jian   

  1. Shenyang Center of Geological Survey,China Geological Survey, Shenyang, Liaoning 110034,China
  • Received:2018-08-06 Revised:2018-11-19 Online:2019-05-08 Published:2019-05-08

摘要:

沉积岩的地球化学特征蕴含了大量的地质信息,对于沉积环境的重塑及物源研究具有重要意义。通过对辽宁北部秀水盆地秀D1井义县组泥岩样品常量、微量及稀土元素等地球化学特征的研究表明:泥岩样品轻稀土元素富集,重稀土元素亏损严重,配分曲线“右倾”,可见中等Eu负异常和微弱的Ce负异常,指示稳定的上地壳物源注入。盆地北东—东部的侏罗系、二叠系酸性侵入岩与义县组沉积岩具有较好的亲缘性,可能为其主要物源,源区构造背景主要为活动大陆边缘。B、Sr/Ba、LaN/SmN、V/(V+Ni)、Fe2+/Fe3+、Cu/Zn及Ceanom等地球化学指标表明义县组沉积时期为淡水环境,古沉积环境为深水还原环境。

关键词: 秀水盆地, 义县组, 秀D1井, 地球化学, 沉积环境, 物源, 构造背景

Abstract:

The geochemical characteristics of sedimentary rocks contain a large amount of geological information, which is of great significance for restoring the sedimentary environments and the provenances. Through the analysis on geochemical characteristics such as major, trace elements and REE of mudstone samples of the Yi-xian Formation from Well Xiu-D1, the results show: REE in mudstones are enriched of LREE with a deficit of HREE. The REE patterns incline to the right, with slightly negative Ce anomalies and moderately negative Eu anomalies, indicates stable provenance input from upper continental crust. The acidic intrusive rocks of the Jurassic and Permian in the northeast-east part of the basin have a great affinity with sedimentary strata of the Yixian Formation,so acidic intrusive are highly likely to be provenance of sedimentary strata. The tectonic setting of provenance area is mainly active continental margin. The geochemical indicators such as B, Sr/Ba, LaN/SmN,V/(V+Ni), Fe2+/Fe3+, Cu/Zn and Ceanom indicate that the Yixian Formation was deposited in fresh, deep water with a reductive environment.

Key words: Xiushui Basin, Yixian Formation, Well Xiu-D1, geochemistry, sedimentary environment, provenance, tectonic setting

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