Geochemical characteristics of elements in sedimentary environment and its geological significance
DOI:
https://doi.org/10.63313/CESS.4008Keywords:
Major elements, Trace elements, Rare earth elements, Geochemical characteristics, Sedimentary environment, Geological significanceAbstract
Elements, especially inorganic elements, are geochemical tracers widely used to study the evolution of various geological processes, material sources and environmental changes, especially in the fields of ocean, environment, mineral deposits and so on. The geochemical characteristics of elements in the sedimentary environment are of great significance for tracing the provenance of sediments. The content of elements changes with the change of rock type, sedimentary process and sedimentary environment. Some elements with relatively stable chemical properties are basically not affected by the weathering, denudation, redeposition and diagenesis of rocks, and can well reflect the provenance characteristics of source rocks. Other elements have different characteristics in different sedimentary environments. Some elements are enriched in marine sediments, while others are enriched in terrigenous sediments, and are affected by sedimentary fluid environment in this process. For example, the enrichment degree of some metal elements will also change in different oxidation-reduction environments. With the process of sedimentary evolution, trace elements will also be dispersed and enriched during the formation, sedimentation and burial of sedimentary organic matter. Therefore, the analysis of the geochemical characteristics of elements in the sedimentary environment is of great significance for identifying the provenance and tectonic setting of sediments.
References
[1] Cheng Y, Yu X, Han B, et al. Geochemical characteristics of the 3rd Member of Paleogene Shahejie Formation in Dongpu Depression and their geological implications[J]. Geology in China. 2010, 37(2): 357-366.
[2] Yin J, Wang Q, Hao F, et al. Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin[J]. Earth Science. 2017, 42(7): 1209-1222.
[3] Zheng Y, Ma Z, Wang B, et al. Geochemistry characteristics and sedimentary environment of oil shale from the Eocene Bahuli Formation in Liushuhe Basin,Heilongjiang Province[J]. Journal of Palaeogeography(Chinese Edition). 2015, 17(5): 689-698.
[4] Zheng Y, Lei Y, Zhang L, et al. Characteristics of Element Geochemistry and Paleo Sedi-mentary Environment Evolution of Zhangjiatan Shale in the Southeast of Ordos Basin and Its Geological Significance for Oil and Gas[J]. Natural Gas Geoscience. 2015, 26(7): 1395-1404.
[5] Wang S, Dong D, Wang Y, et al. Geochemical Characteristics the Sedimentation Environ-ment of the Gas-enriched Shale in the Silurian Longmaxi Formation in the Sichuan Basin[J]. Bulletin of Mineralogy,Petrology and Geochemistry. 2015, 34(6): 1203-1212.
[6] Bouchez J, Gaillardet J M, France-Lanord C, et al. Grain size control of river suspended sediment geochemistry: Clues from Amazon River depth profiles[J].Geochemistry Geo-physics Geosystems. 2011, 12(3): 1-14.
[7] Maharana C, Srivastava D, Tripathi J K. Geochemistry of sediments of the Peninsular rivers of the Ganga basin and its implication to weathering, sedimentary processes and prove-nance[J]. Chemical Geology. 2018, 483: 1-20.
[8] Yang S, Li C, Wang Z, et al. Heterogeneity of geochemical composition of modern Yangtze River sediments and source tracing[J]. Quaternary Sciences. 2013, 33(4): 645-655.
[9] An Y, Liu J, Zhang J, et al. Comparative Study on Source Identification Indicators of Sedi-ments from Huaihe River, Yangtze River and Yellow River[J]. Quaternary Sciences. 2020, 40(3): 837-850.
[10] Hu J, Li Q, Li J, et al. Geochemical Characteristics and Its Application to Depositional Envi-ronment Analysis of Permian Carbonates in Jiaomuri Area, Qiangtang Basin[J]. Geological Journal of China Universities. 2014, 20(4): 520-527.
[11] Shen L, Liu C,Wang L. Geochemical Characteristics of Rare Earths and Trace Elements,of the Upper Yunlong Formation in Lanping Basin,Yunnan and Its Environments Signifi-cance[J]. Acta Geologica Sinica. 2015, 89(11): 2036-2045.
[12] Graham S and Peter S. Diagenetic constraints on the use of cerium anomalies as pal-aeoseawater redox proxies: an isotopic and REE study of Cambrian phosphorites[J]. Chemical Geology. 2001, 175(1) : 29-48.
[13] Wang Y, Li R, Gao S, et al. Trace element characteristics and sedimentary environment of lacustrine carbonate rocks in the Huanghua Depression, Bohai Bay Basin[J]. Petroleum Ge-ology & Experiment. 2017, 39(06): 849-857.
[14] Jia Z, Hou D, Sun D, et al. Characteristics and geological implications of rare earth elements in black shale in hydrothermal sedimentation areas: A case study from the Lower Cam-brian Niutitang Fm shale in central and eastern Guizhou[J]. Natural Gas Industry. 2018, 38(05): 44-51.
[15] Cheng J, Zheng L. Sedimentary geochemical characteristics of the Early Cambrian source rocks in Well Jinye 1 in southern Sichuan Basin[J]. Oil & Gas Geology. 2020, 41(4): 800-810.
Downloads
Published
Issue
Section
License
Copyright (c) 2025 by author(s) and Erytis Publishing Limited.

This work is licensed under a Creative Commons Attribution 4.0 International License.