Geochemical background and anomaly characteristics of copper in soils of Mexico on a global scale

Chunyan YAO, Hantao JIANG, Yiping ZHU, Lu ZHENG, Hanwu LI, Tiangang WANG, Jun’an LIU, Luna JESUS Uribe

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Earth Science Frontiers ›› 2025, Vol. 32 ›› Issue (1) : 236-243. DOI: 10.13745/j.esf.sf.2024.10.42

Geochemical background and anomaly characteristics of copper in soils of Mexico on a global scale

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Abstract

Mexico is a major economic power in Latin America and an important mineral producer in the world. Based on data obtained from Mexico global-scale geochemical mapping using 287 deep soil (C layer) samples, this paper produced a C-layer copper geochemical map with a scale of 1∶8000000. The geochemical background and spatial distribution characteristics of copper in soil were studied from a global-scale perspective, and the major copper geochemical anomalies of Mexico were delineated. The main findings are: (1) the copper content in soils of Mexico ranged from 3.6 to 129.0 μg/g, with the mean and median values being 20.3 and 15.9 μg/g, respectively, and the background value being 15.6 μg/g. The Chiapas Plateau and the Southern Madre Island Arc had significantly higher median copper content than other tectonic units, and had the highest background copper value in the whole country. (2) The geochemical map showed uneven distribution of copper content in soil, with the general trend of high in the south, low in the north, and high in the west, low in the east. (3) The geochemical map identified ten copper geochemical anomalies, eight of which reached mega-province scale and two reached province scale. Based on the fit between copper geochemical information and existing mineral deposits, it is considered that the Sierra Madre del Sur and Chiapas Mountains in southern Mexico are important prospective areas for copper in Mexico.

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global-scale / soil / geochemical background / anomaly character / copper / Mexico

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Chunyan YAO , Hantao JIANG , Yiping ZHU , et al . Geochemical background and anomaly characteristics of copper in soils of Mexico on a global scale. Earth Science Frontiers. 2025, 32(1): 236-243 https://doi.org/10.13745/j.esf.sf.2024.10.42

References

[1]
王学求, 谢学锦, 张本仁, 等. 地壳全元素探测: 构建“化学地球”[J]. 地质学报, 2010, 84(6): 854-864.
[2]
王学求. 全球地球化学基准: 了解过去, 预测未来[J]. 地学前缘, 2012, 19(3): 7-18.
[3]
王学求, 周建, 徐善法, 等. 全球地球化学基准网建立与土壤地球化学基准值特征[J]. 中国地质, 2016, 43: 1469-1480.
[4]
SMITH D B, CANNON W F, WOODRUFF L, et al. History and progress of the North American soil geochemical landscapes project, 2001-2010[J]. Geoscience Frontiers, 2012, 19: 19-32.
[5]
姚春彦, 郭维民, 丁海峰, 等. 墨西哥北部拉拉米期斑岩型铜矿床时空分布及典型矿床特征[J]. 地质论评, 2023, 69(1): 383-395.
[6]
CENTENO-GARCÍA E. Mesozoic tectono-magmatic evolution of Mexico: an overview[J]. Ore Geology Reviews, 2017, 81: 1035-1052.
[7]
王素平, 王绘清, 吕晓东, 等. 墨西哥地质、矿产及矿业经济概况[J]. 安徽地质, 2012, 22(4): 273-277, 280.
[8]
SEDLOCK R L, ORTEGA-GUTIÉRREZ F, SPEED R C. Tectonostratigraphic terranes and tectonic evolution of Mexico[J]. Geological Society of America Special Papers, 1993, 278: 1-153.
[9]
梅燕雄, 裴荣富, 杨德凤, 等. 全球成矿域和成矿区带[J]. 矿床地质, 2009, 28(4): 383-389.
[10]
张伟波, 叶锦华. 环太平洋成矿域主要铜-金矿床地质特征、成矿作用及找矿潜力[J]. 地质通报, 2017, 36(1): 1-15.
[11]
王翠芝, 雷华, 姚仲友, 等. 墨西哥中—新生代成矿系列和成矿带划分及其大地构造意义[J]. 地质通报, 2017, 36(12): 2116-2123.
[12]
鄢明才, 迟清华, 顾铁新, 等. 中国各类沉积物化学元素平均含量[J]. 物探与化探, 1995, 19(6): 465-472.
[13]
黄加忠, 杨明龙, 王晓龙, 等. 四川省瓦岗地区水系沉积物地球化学特征及找矿方向[J]. 华东地质, 2024, 45(3): 332-344.
[14]
何清, 魏路, 肖永红. 基于多源数据的土壤侵蚀时空变化分析: 以安徽省宿松县为例[J]. 华东地质, 2023, 44(3): 333-344.
[15]
谢学锦, 刘大文, 向运川, 等. 地球化学块体: 概念和方法学的发展[J]. 中国地质, 2002, 29(3): 225-233.
[16]
TITLEY S. Porphyry copper deposit of the American Cordillera[J]. Arizona Geological Society Digest, 1995, 20: 6-20.
[17]
MCDOWELL F W, ROLDÁN-QUINTANA J, CONNELLY J N. Duration of late Cretaceous-early Tertiary magmatism in east-central Sonora, Mexico[J]. Geological Society of America Bulletin, 2001, 113(4): 521-531.
[18]
姚春彦, 姚仲友, 李汉武, 等. 墨西哥西马德雷山脉中—新生代构造、岩浆演化及成矿特征[J]. 地质通报, 2017, 36(12): 2124-2133.
[19]
BARRA F, RUIZ J, VALENCIA V A, et al. Laramide porphyry Cu-Mo mineralization in northern Mexico: age constraints from Re-Os geochronology in molybdenite[J]. Economic Geology, 2005, 100(8): 1605-1616.
[20]
BEJARANO-CARRILLO C, OCHOA-LANDÍN L, DEL RIO-SALAS R, et al. La Caridad Vieja: vestiges of a removed HS-epithermal system in the La caridad porphyry Cu-Mo system, northeastern Sonora, Mexico, based on XRD, SEM, SWIR spectral analysis and U-Pb zircon dating[J]. Journal of South American Earth Sciences, 2020, 104: 102820.
[21]
SANTILLANA-VILLA C, VALENCIA-MORENO M, DEL RIO-SALAS R, et al. Geochemical variations of precursor and ore-related intrusive rocks associated with porphyry copper deposits in Sonora, northwestern Mexico[J]. Journal of South American Earth Sciences, 2021, 105: 102823.
[22]
VALENCIA-MORENO M, IRIONDO A, GONZÁLEZ-LEÓN C. Temporal constraints on the eastward migration of the late Cretaceous-early Tertiary magmatic arc of NW Mexico based on new 40Ar/39Ar hornblende geochronology of granitic rocks[J]. Journal of South American Earth Sciences, 2006, 22(1/2): 22-38.
[23]
VALENCIA V A, NOGUEZ-ALCÁNTARA B, BARRA F, et al. Re-Os molybdenite and LA-ICPMS-MC U-Pb zircon geochronology for the Milpillas porphyry copper deposit: insights for the timing of mineralization in the Cananea district, Sonora, Mexico[J]. Revista Mexicana de Ciencias Geologicas, 2006, 23(1): 39-53.
[24]
BARRA F, VALENCIA V A. Late Cretaceous porphyry copper mineralization in Sonora, Mexico: implications for the evolution of the southwest North America porphyry copper province[J]. Mineralium Deposita, 2014, 49(7): 879-884.
[25]
DEL RIO-SALAS R, OCHOA-LANDÍN L, VALENCIA-MORENO M, et al. New U-Pb and Re-Os geochronology of Laramide porphyry copper mineralization along the Cananea lineament, northeastern Sonora, Mexico: contribution to the understanding of the Cananea copper district[J]. Ore Geology Reviews, 2017, 81: 1125-1136.
[26]
FERRARI L, OROZCO ESQUIVEL T, BRYAN S E, et al. Cenozoic magmatism and extension in western Mexico: linking the Sierra Madre Occidental silicic large igneous province and the Comondú Group with the Gulf of California rift[J]. Earth Science Reviews, 2018, 183: 115-152.
[27]
CAMPRUBI A. Tectonic and metallogenetic history of Mexico[J]. Society of Economic Geologists, Special Publication, 2013, 17: 201-243.

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