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现代地质 ›› 2021, Vol. 35 ›› Issue (05): 1459-1470.DOI: 10.19657/j.geoscience.1000-8527.2021.039

• 地球化学 • 上一篇    下一篇

基于微量元素岩性地球化学基因的构建与检验

黎介1(), 刘宁强1, 龚庆杰1(), 吴轩2, 严桃桃3   

  1. 1.中国地质大学(北京) 地球科学与资源学院,北京 100083
    2.中国地质调查局 发展研究中心,北京 100037
    3.自然资源部地球化学探测重点实验室,中国地质科学院地球物理地球化学勘查研究所,河北 廊坊 065000
  • 收稿日期:2020-12-16 修回日期:2021-03-01 出版日期:2021-10-10 发布日期:2021-11-04
  • 通讯作者: 龚庆杰
  • 作者简介:龚庆杰,男,教授,博士生导师,1972年出生,地球化学专业,主要从事元素地球化学和勘查地球化学的教学与科研工作。Email: qjiegong@cugb.edu.cn
    黎 介,男,硕士研究生,1997年出生,资源与环境专业,主要从事地球化学方面的研究工作。Email: jieli@cugb.edu.cn
  • 基金资助:
    中央高校基本科研业务费专项(2652018285);自然资源部地球化学探测重点实验室开放基金资助课题

Construction and Test of a Geochemical Lithogene Based on Trace Elements: Case Studies on Weathering Profiles in China

LI Jie1(), LIU Ningqiang1, GONG Qingjie1(), WU Xuan2, YAN Taotao3   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
    2. Development and Research Center, China Geological Survey, Beijing 100037, China
    3. Key Laboratory of Geochemical Exploration, Institute of Geophysical and Geochemical Exploration, CAGS, Langfang, Hebei 065000, China
  • Received:2020-12-16 Revised:2021-03-01 Online:2021-10-10 Published:2021-11-04
  • Contact: GONG Qingjie

摘要:

地球化学基因是近年来提出的新技术。在分析地球化学基因构建方法的基础上提出一种基于微量元素的岩性地球化学基因,并将其编号为LG03,其基因链元素序列为Nb→Ti→Zr→Cr→La→V→Pb→Co→U→Ni→Th。分别选择发育在广东连阳花岗岩与佛冈花岗岩的2个花岗岩风化剖面、海南文昌3个玄武岩风化剖面、北京房山1个花岗闪长岩风化剖面、胶东2个花岗岩风化剖面与1个玄武岩风化剖面及1个花岗闪长岩风化剖面共计10个风化剖面对新构建的LG03基因以及以前基于主量和微量元素混合构建的LG01岩性基因进行检验。采用基因相似度≥80%作为样品之间具有相似基因的判别标准来检验地球化学基因在风化过程中的稳定性时,发现基于微量元素的LG03岩性基因与基于主量和微量元素混合的LG01岩性基因在遗传性与继承性方面基本相似,但LG03基因相对于LG01基因更稳定。采用酸性相似度20%和80%作为划分类基性成分、类中性成分和类酸性成分的标准时,发现LG03和LG01岩性基因在成分分类与物源示踪等方面也基本相似。在物源示踪方面LG03基因相对于LG01基因更稳定;在成分分类方面当二者划分结果不一致时应以LG01基因的酸性相似度划分结果为准,可进一步以LG03基因的划分结果加以约束。在风化、搬运与沉积过程中,地质样品的主量成分可能会受到风成沙、生物体等介质的加入而发生明显改变,进而导致LG01基因发生改变。但这些较单一成分物质的加入并不影响相对不活动微量元素之间的相互关系,从而可使LG03基因保持较好的稳定性。因此相对于LG01基因而言,LG03基因由于消除了受风成沙、生物体等介质的影响而可能具有更广泛的应用领域。

关键词: 地球化学基因, 风化剖面, 基因相似度, 成分分类, 物源示踪

Abstract:

Geochemical gene is a new technique presented in recent years. According to the construction steps of a geochemical gene, a new lithogene labelled LG03 was proposed based on trace elements on the sequence of Nb→Ti→Zr→Cr→La→V→Pb→Co→U→Ni→Th with the standardized reference values of 14.5, 4,016, 147, 81, 35, 130, 19, 24, 1.2, 32, and 5.72, respectively in μg/g. The LG03 lithogene along with the LG01 lithogene which was constructed formerly on major oxides and trace elements were tested on 10 weathering profiles including 4 profiles developed over granitic intrusions, 4 profiles formed on basaltic strata, and 2 profiles developed on granodioritic intrusions in Guangdong Province, Hainan Province, Shandong Province, and Beijing City in China. According to the gene similarity value of ≥80% as the criterion to discriminate samples with similar lithogenes, the gene similarity results on 10 weathering profiles indicate that LG03 and LG01 lithogenes all illustrate good steady during rock weathering on the properties of heredity (gene similarity with respect to parent rock) and inheritance (gene similarity with respect to topsoil). Furthermore, according to the acidic similarities (gene similarity with respect to the gene of 10202020202 on LG01 and LG03), samples can be classified into three groups as acidic-like composition with values of ≥80%, intermediate-like composition with values between 75% and 25%, and basic-like composition with values ≤20%. That is to say, LG03 and LG01 have similar effects on composition classification and provenance discrimination. However, LG03 is more stable than LG01 in the properties of heredity and inheritance and the application on provenance discrimination. When the results of compositional classification on LG03 and LG01 are different, the results on LG01 are recommended and the results on LG03 are also helpful for a further constraint. The concentrations of major oxides (such as SiO2, CaO, P2O5, etc.) in geological materials will be changed clearly resulted from the addition of aeolian sands, organisms, etc. during the weathering, transportation, sedimentation processes. Therefore, the LG01 lithogene which was constructed on both major oxides and trace elements may be unstable while the LG03 lithogene constructed only on relative immobile trace elements may illustrate good stability during the geological processes. Hence, the LG03 lithogene may have wider application fields than LG01 lithogene because of the elimination of addition or dilution effects in geological materials.

Key words: geochemical lithogene, weathering profile, gene similarity, compositional classification, provenance discrimination

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