华北东部中生代高Mg#闪长岩与壳幔相互作用

doi:10.3799/dqkx.2025.195

华北东部中生代高Mg#闪长岩与壳幔相互作用

doi: 10.3799/dqkx.2025.195

1. 中国地质大学地球科学学院地质过程与成矿预测全国重点实验室，湖北武汉，430074
2. 山东鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队)，山东济宁，272100

基金项目:

国家重点研究发展计划(2023YFF0804200)，国家自然科学基金项目(42273023)，中国地质大学武汉教学实验室开放基金(SKJ2024001)

详细信息

作者简介:
辛梦荷（2000-），女，硕士研究生，地球化学专业，E-mail：xinmenghe@163.com ORCID：0009-0006-6557-8382

通讯作者:
汪在聪(1985-)，男，教授，亲铜元素地球化学、行星增生演化与壳幔相互作用，E-mail：zaicongwang@cug.edu.cn ORCID：0000-0002-3584-1673

中图分类号: P581
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出版历程
- 收稿日期: 2025-07-28
- 网络出版日期: 2025-10-15

Shandong Provincial Lunan Geology and Exploration Institute

摘要

摘要: 华北东部在中生代时期发生了强烈的克拉通破坏，并伴随构造-岩浆-成矿活动。在破坏峰期，鲁西-徐淮-大别等地区广泛发育了与同期铁铜金等多种金属成矿有关的高Mg#闪长岩。尽管岩石成因已有大量研究，但是其空间分布规律与岩石圈演化之间的联系仍缺乏系统认识。本文选取华北东部为研究区，系统梳理总结了高Mg#闪长岩的岩相学、时空分布规律、Sr-Nd-Pb同位素特征，构建了大区域尺度纵向空间上的联系，探讨壳幔相互作用中岩石圈的演化过程，为研究区成岩成矿作用以及空间差异性提供重要基础。这些高Mg#闪长岩具有一致的岛弧型微量元素特征及富集的Sr-Nd同位素特征，表明源区存在再循环地壳物质。而且，Sr-Nd-Pb同位素存在空间的显著变化：自南向北，闪长岩(⁸⁷Sr/⁸⁶Sr)_i逐渐降低（0.7117 ~ 0.7043），ε_Nd(t)逐渐升高（-24.90 ~ -1.77），表明了壳源物质对岩石圈地幔改造的程度从南到北逐渐减弱的趋势，支持三叠纪时期扬子大陆板块的俯冲对华北地幔的影响。另一方面，低(⁸⁷Sr/⁸⁶Sr)_i闪长岩具有低的(²⁰⁷Pb/²⁰⁴Pb)_i和(²⁰⁸Pb/²⁰⁴Pb)_i，与华北古老变质基底相似的Pb同位素，说明源区还存在华北古老地壳物质，可能与地壳拆沉有关。因此，高Mg#闪长岩反映出华北东部岩石圈地幔自南向北受再循环物质（扬子地壳）改造程度逐渐减弱并伴随华北地壳拆沉，以及俯冲的扬子地壳和拆沉的华北古老地壳物质对地幔性质改造的不同程度贡献。这也为更好的理解高Mg#闪长岩的形成、演化以及矿床的种类和分布规律提供了重要基础。
- 华北克拉通 /
- 高Mg#闪长岩 /
- 中生代 /
- 壳幔相互作用 /
- 成矿
Abstract: Intense cratonic destruction occurred in the eastern part of the North China Craton (NCC) during the Mesozoic, accompanied by tectonic-magmatic-metallogenic activities. During the peak period of destruction, high Mg# diorites related to the coeval formation of various metal deposits such as iron, copper and gold were widely distributed in regions like Luxi-Xuhuai-Dabie. Although there have been many studies on the genesis of rocks, the connection between the spatial distributions of high Mg# diorites and the evolution of the lithosphere still lacks systematic understanding. This paper selects the eastern part of the NCC as the study area. It comprehensively sorts out and summarizes the petrography, temporal and spatial distribution patterns, and Sr-Nd-Pb isotopic characteristics of high Mg# diorites, establishes the vertical connection on a large regional scale, and explores the evolution process of the lithosphere in the crust-mantle interaction, providing an important basis for magmatic and mineralization processes as well as spatial differences. These high Mg# diorites have consistent island arc-like trace element characteristics and enriched Sr-Nd isotope compositions, indicating the existence of recycled crustal materials in the source region. Moreover, there are significant spatial variations in the Sr-Nd-Pb isotopes: from south to north, the (⁸⁷Sr/⁸⁶Sr)_i of diorites gradually decreased (0.7117 ~ 0.7043), and the ε_Nd(t) gradually increased (-24.90 ~ -1.77), indicating a trend of decreasing influence of crustal materials on the mantle from south to north, which supports the influence of the subduction of the Yangtze continental Plate during the Triassic on the lithospheric mantle beneath the NCC. On the other hand, the low (⁸⁷Sr/⁸⁶Sr)_i diorites have low (²⁰⁷Pb/²⁰⁴Pb)_i and (²⁰⁸Pb/²⁰⁴Pb)_i like those of the ancient metamorphic basement of the NCC, indicating that there are also ancient NCC crustal materials in the source, which may be related to the lower crust delamination. Therefore, the high Mg# diorites reflect that the degree of modification of the lithospheric mantle from south to north by recycled materials (Yangtze crust) gradually weakens, accompanied by the crustal delamination beneath the eastern NCC, and the relative contributions of the subducting Yangtze crust and the NCC ancient crust. This also promotes a better understanding of the formation and evolution of high Mg# diorites, as well as the types and distribution patterns of deposits.
- NCC /
- high-Mg# diorite /
- Mesozoic /
- crust-mantle interaction /
- mineralization

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华北东部中生代高Mg#闪长岩与壳幔相互作用

doi: 10.3799/dqkx.2025.195

作者简介:
辛梦荷（2000-），女，硕士研究生，地球化学专业，E-mail：xinmenghe@163.com ORCID：0009-0006-6557-8382

通讯作者:
汪在聪(1985-)，男，教授，亲铜元素地球化学、行星增生演化与壳幔相互作用，E-mail：zaicongwang@cug.edu.cn ORCID：0000-0002-3584-1673

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Shandong Provincial Lunan Geology and Exploration Institute

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留言板

华北东部中生代高Mg#闪长岩与壳幔相互作用

doi: 10.3799/dqkx.2025.195

作者简介: 辛梦荷（2000-），女，硕士研究生，地球化学专业，E-mail：xinmenghe@163.com ORCID：0009-0006-6557-8382

通讯作者: 汪在聪(1985-)，男，教授，亲铜元素地球化学、行星增生演化与壳幔相互作用，E-mail：zaicongwang@cug.edu.cn ORCID：0000-0002-3584-1673

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Shandong Provincial Lunan Geology and Exploration Institute

计量

出版历程

目录

作者简介:
辛梦荷（2000-），女，硕士研究生，地球化学专业，E-mail：xinmenghe@163.com ORCID：0009-0006-6557-8382

通讯作者:
汪在聪(1985-)，男，教授，亲铜元素地球化学、行星增生演化与壳幔相互作用，E-mail：zaicongwang@cug.edu.cn ORCID：0000-0002-3584-1673