...
首页> 外文期刊>Precambrian Research >Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation
【24h】

Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation

机译:U-Pb年龄和元古生界静二榆组碎屑锆石的Hf同位素揭示了华北克拉通东部前寒武纪地壳演化

获取原文
获取原文并翻译 | 示例
           

摘要

Simultaneous in situ U-Pb dating, trace element and Hf isotopic analyses have been carried out on detrital zircons obtained from sandstones in the Neoproterozoic Jing'eryu Formation from the Eastern Block, North China Craton (NCC), with the aim of constraining the ages of magmatic and metamorphic events and hence the Precambrian crustal evolution of the NCC. Two groups of zircons, i.e., magmatic and metamorphic in origin, have been identified based on cathodoluminescence images, zircon Ti-temperatures and Th/U ratios. Zircon U-Pb dating shows two main magmatic events with ages of 2.55-2.47. Ga and 1.80-1.70. Ga, and four metamorphic events, with ages of 2.51-2.48. Ga, 1.96-1.90. Ga, 1.87-1.85. Ga and ~1.80. Ga in the NCC. No zircons with ages of ~3.8. Ga have been identified in this study, indicating either these were covered at the time of deposition or the limited presence of 3.8. Ga rocks in the NCC. The Hf isotopic data show the ~2.5Ga magmatic zircons have variable e{open} _(Hf)(t) values, including both positive and negative values and with crustal model ages of 2.7-2.9Ga, which can be interpreted to indicate mixed sources for their parental rocks, i.e., ancient crust (3.8Ga or 3.3Ga) and depleted mantle, implying significant continental crustal growth at ~2.5Ga. However, Paleoproterozoic magmatic zircons all have negative e{open} _(Hf)(t) and Archean Hf model ages, suggesting that their parental rocks were formed from recycled Archean materials. The widespread ~2.5. Ga metamorphism in the Eastern Block, coupled with extensive ~2.5. Ga magmatism and crustal growth, are consistent with a mantle plume beneath the Eastern Block of the NCC during the Neoarchean. Whereas, a progressive increase in ~1.85. Ga metamorphic zircon westward across the Eastern Block toward the Trans-North China orogen is best explained by collision between the Eastern and Western blocks at this time.
机译:对华北克拉通东部(NCC)东部新元古生界静二榆组砂岩中的碎屑锆石进行了原位U-Pb定年,痕量元素和Hf同位素分析。岩浆和变质事件的发生,从而解释了NC​​C的前寒武纪地壳演化。基于阴极发光图像,锆石的Ti温度和Th / U比,已经鉴定出两组锆石,即起源的岩浆岩和变质岩。锆石U-Pb测年显示出两个主要的岩浆事件,年龄为2.55-2.47。 Ga和1.80-1.70。 Ga和四个变质事件,年龄为2.51-2.48。加,1.96-1.90。 ,1.87-1.85。 Ga和〜1.80。 NCC中的Ga。年龄不超过3.8的锆石。在本研究中已鉴定出Ga,表明在沉积时这些化合物已被覆盖或3.8的有限存在。嘎岩在NCC中。 Hf同位素数据表明,〜2.5Ga岩浆锆石具有可变的e {open} _(Hf)(t)值,包括正值和负值,地壳模型年龄为2.7-2.9Ga,这可以解释为表明混合其亲代岩石的来源,即古老的地壳(3.8Ga或3.3Ga)和地幔枯竭,暗示着〜2.5Ga的大陆地壳显着生长。然而,古元古代岩浆锆石都具有负e(open)_(Hf)(t)和太古宙Hf模型年龄,表明它们的母岩是由太古宙再生材料形成的。普遍〜2.5。东部地带的Ga变质作用,加上广泛的〜2.5。伽马岩浆作用和地壳生长,与新archarean时期NCC东区下方的地幔柱相吻合。而〜1.85逐渐增加。最好的解释是,此时东部和西部地块之间的碰撞可以很好地解释Ga变质锆石向西穿过东部地块向华北华北造山带的作用。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号