Two stages of late Paleoproterozoic A-type granites at the southern North China Craton: Geochemical constraints and implications for supercontinent breakup

IF 3.2 2区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Zhiyi Wang , Jingxin Zhao , Zeqiu Qi , Dongyang Huo , Wolfgang Siebel , Jun He , Shuangqing Li , Fukun Chen
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Abstract

Paleoproterozoic and Mesoproterozoic A-type granites occur on many cratons and possess important information for our understanding of the formation and breakup history of the supercontinent Columbia. It was argued previously, that Proterozoic A-type granites (∼1.8–1.5 Ga), exposed along the southern margin of the North China Craton formed in a post-collisional or anorogenic setting related to the final amalgamation of the North China Craton or to the breakup of Columbia. In the present study, we report zircon ages and geochemical data of the Maping A-type granite. This intrusion consists of a quartz monzonite porphyry and a granite porphyry that, based on U-Pb age dating, formed at ∼ 1.65 and ∼ 1.60 Ga, respectively. The granites show high contents in alkaline and high field strength elements, high Ga/Al and Fe/Mg ratios. The quartz monzonite porphyry of the early stage is metaluminous and relatively depleted in Hf-Nd isotopic compositions (whole-rock initial εNd values −5.4 to −4.5; zircon initial εHf values −8.5 to −1.5), while granite porphyry of the late stage is peraluminous and has lower initial εNd and εHf values (−6.4 to −5.9; −9.6 to −3.3). Inherited zircon grains in the Maping intrusion have relatively high initial εHf values (>-0.7), likely originating from juvenile crust. The Pb isotopes of the quartz monzonite porphyry show characteristics similar to the lower crust, whereas the granite porphyry has more radiogenic Pb isotopic compositions. Apatite grains from the quartz monzonite porphyry have initial 87Sr/86Sr ratios of ∼ 0.7109–0.7133 and those from the granite porphyry have noticeably high initial 87Sr/86Sr ratios of ∼ 0.7862–0.8812. These isotopic characteristics imply the presence of various crustal rocks underneath the North China Craton with variable isotopic compositions. From the early to late magmatic stages, the Sr/Y ratios of granitic rocks decrease from 1.6 – 7.6 to 0.2–0.4, while the estimated magma temperatures, calculated from whole-rock compositions, slightly increase from approximately 900 °C to about 930 °C. These concurrent changes in temperature and chemical composition reflect ongoing asthenospheric mantle upwelling during crustal extension. This suggests a transition in the southern margin of the North China Craton from a post-collisional setting before 1.65 Ga to an anorogenic setting by 1.6 Ga.

华北克拉通南部晚古生代A型花岗岩的两个阶段:地球化学制约因素及其对超大陆解体的影响
古近纪和中新生代A型花岗岩分布在许多克拉通上,对于我们了解哥伦比亚超大陆的形成和解体历史具有重要意义。此前有观点认为,华北克拉通南缘出露的新生代A型花岗岩(1.8~1.5 Ga)形成于碰撞后或与华北克拉通最终汞齐化或哥伦比亚断裂有关的成因环境中。在本研究中,我们报告了马平A型花岗岩的锆石年龄和地球化学数据。该侵入体由一个石英单斜斑岩和一个花岗斑岩组成,根据U-Pb年龄测定,分别形成于∼ 1.65 Ga和∼ 1.60 Ga。这些花岗岩显示出较高的碱性和高场强元素含量、较高的镓/铝和铁/镁比率。早期的石英斑岩为金属铝质,Hf-Nd同位素组成相对贫乏(全岩初始εNd值为-5.4至-4.5;锆石初始εHf值为-8.5至-1.5);晚期的花岗斑岩为过铝质,初始εNd和εHf值较低(-6.4至-5.9;-9.6至-3.3)。马平侵入体中的继承锆石晶粒具有相对较高的初始εHf值(>-0.7),可能源自幼壳。石英斑岩的铅同位素显示出与下地壳相似的特征,而花岗斑岩的铅同位素组成则更具放射性。石英单斜斑岩中的磷灰石颗粒的初始 87Sr/86Sr 比率为 0.7109-0.7133 ∼,而花岗斑岩中的磷灰石颗粒的初始 87Sr/86Sr 比率明显较高,为 0.7862-0.8812 ∼。这些同位素特征意味着华北克拉通地下存在着不同同位素组成的地壳岩石。从早期岩浆阶段到晚期岩浆阶段,花岗岩的Sr/Y比值从1.6-7.6下降到0.2-0.4,而根据全岩成分计算的估计岩浆温度略有上升,从约900 °C上升到约930 °C。这些温度和化学成分的同时变化反映了地壳延伸过程中持续的星体层地幔上涌。这表明华北克拉通南缘已从1.65 Ga之前的碰撞后环境过渡到1.6 Ga之前的原生环境。
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来源期刊
Precambrian Research
Precambrian Research 地学-地球科学综合
CiteScore
7.20
自引率
28.90%
发文量
325
审稿时长
12 months
期刊介绍: Precambrian Research publishes studies on all aspects of the early stages of the composition, structure and evolution of the Earth and its planetary neighbours. With a focus on process-oriented and comparative studies, it covers, but is not restricted to, subjects such as: (1) Chemical, biological, biochemical and cosmochemical evolution; the origin of life; the evolution of the oceans and atmosphere; the early fossil record; palaeobiology; (2) Geochronology and isotope and elemental geochemistry; (3) Precambrian mineral deposits; (4) Geophysical aspects of the early Earth and Precambrian terrains; (5) Nature, formation and evolution of the Precambrian lithosphere and mantle including magmatic, depositional, metamorphic and tectonic processes. In addition, the editors particularly welcome integrated process-oriented studies that involve a combination of the above fields and comparative studies that demonstrate the effect of Precambrian evolution on Phanerozoic earth system processes. Regional and localised studies of Precambrian phenomena are considered appropriate only when the detail and quality allow illustration of a wider process, or when significant gaps in basic knowledge of a particular area can be filled.
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