华北克拉通东部白垩纪玄武岩的成因及源区变化：Sr-Nd-Pb同位素的证据
Genesis and Source Area Variations of Cretaceous Basalts in Eastern North China Craton: Evidence of Sr-Nd-Pb Isotopes
DOI: 10.12677/AG.2022.128108, PDF,   
作者: 郭喜慧：哈尔滨师范大学，黑龙江 哈尔滨
关键词: 玄武岩；太平洋板块；华北克拉通；岩石圈减薄；Basalt； Pacific Plate； North China Craton； Lithosphere Thinning
摘要: 白垩纪被认为是华北克拉通破坏的峰期，这一时期伴随有大量火山岩的喷发。大陆玄武岩的地球化学组成通常被认为是大陆岩石圈化学和同位素演化的最佳记录。其主要以碱性玄武岩为主，亚碱性玄武岩较少。这些玄武岩的化学成分和同位素组成的突变往往归因于其东部岩石圈的减薄。然而，造成这种突变的过程及其对大陆岩石圈演化的影响仍然不清楚。本文通过对华北克拉通东部白垩纪玄武岩的Sr-Nd-Pb同位素分析提出：大于108 Ma碱性玄武岩的εNd(t)值自东向西呈负向变化，具有岛弧递减的地球化学特征，暗示其交代岩石圈地幔源中来自俯冲板块的成分减少。相反，小于108 Ma白垩纪碱性玄武岩具有亏损的Sr-Nd同位素组成和类似OIB地球化学特征。这些观察结果表明，古太平洋板块向西俯冲是华北克拉通白垩纪玄武岩活动的主要原因。结合板块构造和地球物理的观察，我们认为古太平洋板块的平俯冲控制这些地球化学特征的变化以及华北克拉通的破坏，108 Ma的转变可能由于板片回卷造成的。
Abstract: The Cretaceous period is thought to be the peak of the north China Craton’s destruction, accompanied by massive volcanic eruptions. The geochemical composition of continental basalts is generally regarded as the best record of the chemical and isotopic evolution of the continental lithosphere. It is mainly alkaline basalt, sub alkaline basalt is less. Abrupt changes in the chemical and isotopic composition of these basalts are often attributed to thinning of the eastern lithosphere. However, the process that caused this mutation and its impact on the evolution of the continental lithosphere remains unclear. Based on the Sr-Nd-Pb isotopic analysis of cretaceous basalts in the eastern North China Craton, the εNd(t) values of alkaline basalts greater than 108 Ma show a negative change from east to west, showing the geochemical characteristics of island arc decline, suggesting that the metasomatic lithospheric mantle source is less derived from subduction plate. In contrast, cretaceous alkaline basalts less than 108 Ma have depleted Sr-Nd isotopic composition and OIB-like geochemical characteristics. These observations indicate that the westward subduction of the Paleo-Pacific plate was the main cause of cretaceous basalt activity in the North China Craton. Combined with the observations of plate tectonics and geophysics, we believe that the flat subduction of the Paleo-Pacific plate controlled the changes of these geochemical characteristics and the destruction of the North China Craton, and that the 108 Ma transition may have been caused by plate rewind.
文章引用：郭喜慧. 华北克拉通东部白垩纪玄武岩的成因及源区变化：Sr-Nd-Pb同位素的证据[J]. 地球科学前沿, 2022, 12(8): 1117-1126. https://doi.org/10.12677/AG.2022.128108

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