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富有机质样品Re-Os同位素定年实验方法

武鲁亚 金之钧 储著银 刘可禹

武鲁亚, 金之钧, 储著银, 刘可禹. 富有机质样品Re-Os同位素定年实验方法[J]. 石油实验地质, 2021, 43(3): 513-523. doi: 10.11781/sysydz202103513
引用本文: 武鲁亚, 金之钧, 储著银, 刘可禹. 富有机质样品Re-Os同位素定年实验方法[J]. 石油实验地质, 2021, 43(3): 513-523. doi: 10.11781/sysydz202103513
WU Luya, JIN Zhijun, CHU Zhuyin, LIU Keyu. Re-Os isotopic dating procedures for organic-rich samples[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(3): 513-523. doi: 10.11781/sysydz202103513
Citation: WU Luya, JIN Zhijun, CHU Zhuyin, LIU Keyu. Re-Os isotopic dating procedures for organic-rich samples[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(3): 513-523. doi: 10.11781/sysydz202103513

富有机质样品Re-Os同位素定年实验方法

doi: 10.11781/sysydz202103513
基金项目: 

中国科学院战略性先导科技专项A类项目 XDA14010401

中国石油大学(华东)自主创新科研计划 17CX06032

详细信息
    作者简介:

    武鲁亚(1993-), 女, 博士研究生, 从事地球化学和油气成藏年代学研究。E-mail: b16010016@s.upc.edu.cn

    通讯作者:

    刘可禹(1963-), 男, 教授, 从事沉积学与石油地质学等研究。E-mail: liukeyu@upc.edu.cn

  • 中图分类号: TE135

Re-Os isotopic dating procedures for organic-rich samples

  • 摘要: 近年来,铼—锇(Re-Os)同位素体系在确定含油气系统烃源岩沉积年龄、烃类生成、运移、后期调整改造年龄(古油藏热裂解、硫酸盐热化学还原反应等)以及油源示踪方面取得了一系列成果。但是,富有机质样品的Re-Os同位素体系存在元素丰度低、赋存形式复杂、同位素体系封闭性影响因素以及Os同位素组成均一机制不清等诸多难题,进而导致其构建的等时线年龄误差相对较大。通过测年样品筛选、富有机质样品化学前处理、实验流程空白控制以及国际参考标样监控等4个方面,对现有的富有机质样品的Re-Os同位素分析测试全流程进行了总结与完善,可为拟开展含油气系统Re-Os定年工作的研究人员提高数据质量,构建理想的Re-Os等时线。

     

  • 图  1  国外典型含油气系统原油样品Re-Os同位素等时线

    a.英国Shetland群岛原油(原始数据引自文献[11]);b.美国Bighorn盆地Phosphoria原油(原始数据引自文献[12])

    Figure  1.  Re-Os isochrons of crude oil samples from two typical petroleum systems abroad

    图  2  意大利Ragusa盆地Gela-1井原油样品Re-Os同位素等时线

    a.Noto和Sciacca组的全油和沥青质组分;b.Streppenosa组原油可溶组分(马青烯)(原始数据引自文献[16])

    Figure  2.  Re-Os isochrons of crude oil from well Gela-1 in Ragusa Basin, Italy

    图  3  富有机质样品Re-Os同位素分析完整实验流程

    Figure  3.  Procedure for determining Re-Os concentrations and isotopic compositions of organic-rich samples

    图  4  不同实验测定的NIST8505原油标样的Re含量(a)、Os含量(b),187Re/188Os(c)和187Os/188Os比值(d)

    图a和图b中灰色虚线为不同实验室测定数据的平均值;图中红色实线为实验室间平均值,红色虚线表示其各自的2σ标准偏差原始数据引自文献[16, 28, 35, 45, 54-55]。

    Figure  4.  Concentrations of Re (a) and Os (b) and isotopic compositions (c-d) of crude oil standard sample NIST8505 analyzed by three different laboratories

    表  1  国内外Re-Os实验室常用溶样方法比较

    Table  1.   Comparison of commonly used sample digestion methods for Re-Os isotopic analysis

    溶样方法 优点 缺点/局限性
    酸溶法(HBr,HCl-乙醇) 可避免产生挥发性的OsO4,本底低 样品溶解不完全,回收率低
    碱熔法 可完全溶解难熔相 实验本底高,消解过程中难达到同位素交换平衡
    硫化镍火试金法 溶样量大,可有效避免Os的“块金效应” Re的数据可信度较低,Os本底高,溶样过程中存在Os的损失
    Carius管溶样法 密闭体系,样品近完全溶解,易达到同位素交换平衡,本底低 对于一些难溶矿物不能完全溶解,易爆炸
    高温高压反应釜法 完全、快速消解样品,本底低,安全性高 实验装置较为昂贵,溶样管重复利用
    注:表中数据据文献[29-35]整理。
    下载: 导出CSV

    表  2  近几年国内外主要Re-Os实验室全流程Re-Os本底水平对比

    Table  2.   Total analytical blanks of major Re-Os laboratories reported recently

    Re-Os同位素实验室 溶样方法 Re本底水平/pg Os本底水平/pg 187Os/188Os 数据来源
    科罗拉多州立大学 HPA-S逆王水溶样 16.3±16.2 0.102±0.066 0.53±0.31 [16]
    Carius管逆王水溶样 3.7±4.7 0.34±0.226 0.251±0.02 [16]
    HPA-S硝酸溶样 0.98±0.18 0.167±0.024 0.31±0.04 [16]
    杜伦大学 Carius管逆王水溶样 1.63±0.67 0.065±0.013 0.23±0.02 [17]
    Carius管硫酸氧化铬溶样 16.8±0.4 0.4±0.1 0.25±0.21 [21]
    中科院地质与地球物理研究所 Carius管逆王水溶样 7±0.62 0.25±0.12 [41]
    中科院广州地球化学研究所 Carius管逆王水溶样 8.8±3.2 0.28±0.2 0.259±0.038 [48]
    Carius管硫酸氧化铬溶样 0.75±0.32 0.33±0.29 0.206±0.025 [50]
    Carius管H2O2-HNO3溶样 8±3 0.8±0.2 0.128 9± 0.004 8 [50]
    国家地质实验测试中心 Carius管HNO3-HCl-H2O2溶样 2 0.1 [49]
    科廷大学 Carius管逆王水溶样 17 0.54 0.137 ± 0.028 [51]
    下载: 导出CSV
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  • 收稿日期:  2020-09-30
  • 修回日期:  2021-04-16
  • 刊出日期:  2021-05-28

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