Huge growth of the late Mesoarchean–early Neoarchean (2.6~3.0 Ga) continental crust in the North China Craton: A review
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摘要:
在对一些重点地区新太古代早期—中太古代晚期（2.6~3.0 Ga）岩石的空间分布、岩石类型和形成时代作简要介绍基础上，文章总结了华北克拉通这一时代花岗质岩石的年龄分布模式、地球化学和Nd-Hf-O同位素组成特征。新太古代早期—中太古代晚期变质基底具有如下特征：①新太古代早期—中太古代晚期岩浆作用在华北克拉通几乎连续分布，峰期为2.70~2.75 Ga；②新太古代早期—中太古代晚期岩石在华北克拉通广泛存在，主要分布在东部古陆块、中部古陆块和南部古陆块中；③新太古代早期—中太古代晚期侵入岩以英云闪长岩为主，存在奥长花岗岩和花岗闪长岩及其他类型岩石；④新太古代早期—中太古代晚期表壳岩规模很小，零星分布于花岗质岩石中，岩石类型主要为变玄武质岩石，一些地区存在变质科马提岩、变质安山质‒英安质火山岩和变质碎屑沉积岩；⑤2.6 Ga可作为华北克拉通新太古代早期和晚期的界线；⑥TTG岩石的Sr/Y和La/Yb比值存在很大变化，在Sr/Y-Y和La/Yb-Yb图中位于高压、中压和低压TTG分布区；除少量富钾花岗岩外，华北克拉通新太古代早期—中太古代晚期岩石大都具有亏损Nd-Hf同位素组成特征；岩浆锆石O同位素组成与全球太古宙岩浆锆石类似；⑦许多地区都具有类似地质特征，但一些地区显示出较大的独特性。新的研究进一步支持了这样的认识：与全球其他许多典型克拉通类似，新太古代早期—中太古代晚期是华北克拉通最重要的陆壳增生时期，主要区别是华北克拉通叠加了强烈的新太古代晚期岩浆构造热事件。
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关键词:
- 新太古代早期—中太古代晚期 /
- 华北克拉通 /
- Nd-Hf-O同位素 /
- TTG /
- 陆壳巨量增生
Abstract:Based on a brief introduction of the spatial distribution, rock types and formation ages of the late Mesoarchean–early Neoarchean (2.6~3.0 Ga) rocks in some key areas of the North China Craton, this paper summarizes the ages and geochemical and Nd-Hf-O isotopic compositions of the granitoids all over the craton. The late Mesoarchean–early Neoarchean basement shows the following features: (1) The late Mesoarchean–early Neoarchean magmatism is almost continuous, with a peak period of 2.70~2.75 Ga; (2) The late Mesoarchean–early Neoarchean rocks widely occur in the North China Craton, mainly in the Eastern Ancient Terrane, the Central Ancient Terrane and the Southern Ancient Terrane; (3) The intrusive rocks are mainly tonalite in composition, with trondhjemite, granodiorite, K-rich granite and gabbro-diorite; (4) The supracrustal rocks are commonly small in scale and scatter in granitoids. The rock types are mainly meta-basaltic rocks. In some areas, there are meta-komatiites, meta-andesitic-dacitic rocks and meta-clastic sedimentary rocks; (5) 2.6 Ga can be regarded as the boundary between the early and late Neoarchean in the North China Craton; (6) TTG rocks show large Sr/Y and La/Yb variations, plotting in the high-, medium- and low-pressure TTG areas in the Sr/Y–Y and La/Yb–Yb diagrams. Except for a few K-rich granites, the late Mesoarchean–early Neoarchean rocks are commonly depleted in Nd-Hf isotope compositions, with the magmatic zircon being similar in O isotope composition to that of the Archean magmatic zircon worldwide; (7) Many regions have similar geological characteristics, but some regions show great uniqueness. The research futher supports the understanding that, similar to many other typical cratons worldwide, the late Mesoarchean–early Neoarchean is the most important period of continental accretion in the North China Craton, and the main difference is that the North China Craton underwent a strong and widespread magmato-tectonothermal event at the end of the Neoarchean.
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图 2 吉南‒辽北地区地质图（图中给出了2.6~3.0 Ga岩石定年样品分布，据Bao et al.，2022修改）
Figure 2.
图 4 铁架山‒弓长岭地区地质图（底图据Dong et al., 2017a；图中给出了2.9~3.0 Ga富钾花岗岩定年样品位置，数据来源Dong et al., 2017a；王伟等, 2022）
Figure 4.
图 7 冀东地区地质图（底图据Nutman et al., 2011；图中给出了2.6~3.0 Ga 定年岩石样品的位置，数据来源Nutman et al., 2011；Liou et al., 2019)
Figure 7.
图 8 冀东草场地区中太古代表壳岩的野外照片（Liou et al., 2019）
Figure 8.
图 11 白云鄂博‒固阳地区地质图（底图据Jian et al.，2012修改；图中给出了新太古代早期定年岩石样品的位置，数据来源董晓杰等，2012；马铭株等，2013；董春艳等，2021）
Figure 11.
图 14 胶东地区地质图（Wan et al., 2015；图中给出了太古宙岩石定年样品空间分布（栖霞地区除外）和图15的位置）
Figure 14.
图 15 栖霞地区地质图（万渝生等，2017；Wan et al., 2021；图中给出了太古宙定年样品位置，三角、方框和圆圈分别代表2.9 Ga、2.7 Ga和2.5 Ga岩石样品）
Figure 15.
图 16 栖霞地区太古宙岩浆岩的Nd-Hf同位素组成（Wan et al., 2021）
Figure 16.
图 17 胶东莱州地区太古宙岩石的野外照片（万渝生等，2019a）
Figure 17.
图 18 胶东莱州地区太古宙岩石的锆石阴极发光图像和U-Pb谐和图（万渝生等，2019a）
Figure 18.
图 19 鲁西七星台地区地质图（底图据Bai et al., 2020；图中给出了新太古代早期定年样品位置，数据来源马铭株等，2020）
Figure 19.
图 23 蚌埠地区地质图（底图据刘贻灿等，2015；图中给出了中太古代晚期定年样品位置，数据来源Liu et al., 2019）
Figure 23.
图 24 蚌埠地区中太古代晚期花岗质岩石的锆石阴极发光图像和U-Pb谐和图（Liu et al., 2019）
Figure 24.
图 25 鲁山地区地质图（底图据Liu et al., 2009a；图中给出了新太古代早期—中太古代晚期定年样品位置，数据来源Liu et al., 2009a；Diwu et al., 2010；Zhou et al., 2014; Jia et al., 2020）
Figure 25.
图 26 鲁山地区中太古代岩石的野外照片（Liu et al., 2009a）
Figure 26.
图 27 鲁山地区中太古代岩石的锆石阴极发光图像和U-Pb谐和图（Liu et al., 2009a）
Figure 27.
图 31 华北克拉通新太古代早期—中太古代晚期花岗质岩石的Sr/Y-Y和La/Yb-Yb图解（Moyen, 2011）
Figure 31.
图 39 华北克拉通新太古代早期—中太古代晚期花岗质岩石的Nb-Y和Ta-Yb图解（底图据Pearce et al., 1984）
Figure 39.
图 40 华北克拉通大陆地壳生长线（万渝生，2018；不同的全球大陆地壳生长线引自Cawood et al.，2013）
Figure 40.
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