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河北怀安地区桑干岩群岩石组合特征及锆石U-Pb年代学对其形成和变质时代的约束

陈后华 段留安 张平阳 王卫国 宋贺民

地质通报2025,Vol.44Issue(5):872-884,13.
地质通报2025,Vol.44Issue(5):872-884,13.DOI:10.12097/gbc.2023.12.009

河北怀安地区桑干岩群岩石组合特征及锆石U-Pb年代学对其形成和变质时代的约束

Rock association of Sanggan Group from Huai'an region,Hebei Province,and constraints of zircon U-Pb geochronology on their formation and metamorphic ages

陈后华 1段留安 2张平阳 3王卫国 1宋贺民1

作者信息

  • 1. 烟台黄金职业学院,山东 烟台 265401
  • 2. 中国地质调查局烟台海岸带地质调查中心,山东 烟台 264000||自然资源部深部金矿勘查开采技术创新中心/山东省深部金矿探测大数据应用开发工程实验室,山东 威海 264209
  • 3. 中国地质调查局烟台海岸带地质调查中心,山东 烟台 264000
  • 折叠

摘要

Abstract

[Objective]The Precambrian metamorphic basement is widely exposed in the Huai'an area of Hebei Province.Previous studies have proposed different schemes for the stratigraphic division of metamorphic rocks in the Huai'an area.However,the formation and metamorphic ages of these metamorphic rocks remain controversial.[Methods]Through the 1:50,000 regional geological survey in Huai'an area,Hebei Province,the Mashikou Formation and Yousuopu Formation of the Sanggan Group in the Huai'an Complex Belt have been redefined and subdivided based on rock association.The zircon U-Pb age dating of granulites and gneiss of the Sanggan Group was carried out based on in-situ LA-ICP-MS analysis.[Results]The Mashikou Formation is mainly composed of granulites,with occurrences of hypersthene and augite.The rock mass of Mashikou Formation is overall grayish yellow in color,with locally interlayers of magnetite quartzite.Compared to the Mashikou Formation,there is a significant increase in layers of plagioclase amphibolite in the Yousuopu Formation,containing higher proportions of biotite and hornblende,locally interbedded with a small amount of grayish-colored marble veins.Accroding to characteristics of rock association and protolith reconstruction,the protolith of Sanggan Group is mainly composed of ultra-basic and basic volcanic rocks,with a small amount of intermediate acidic volcanic rocks interbedded with muddy clastic,ferro-siliceous,and carbonate sedimentary rocks.It belongs to volcano-sedimentary series which were formed at extensional and passive continental margin basins.The zircon U-Pb dating of granulites and gneiss from Sanggan Group show two age peaks between 2.6~2.2 Ga and 2.0~1.7 Ga.[Conclusions]The rock association and zircon U-Pb age distribution peaks collectively indicate that the protoliths of Sanggan Group in the Huai'an area were formed in the late Neoarchean(~2.5 Ga)and underwent amphibolite-facies to granulite-facies metamorphism in the Late Paleoproterozoic(~1.8 Ga).

关键词

桑干岩群/岩石组合特征/锆石U-Pb定年/LA-ICP-MS/河北怀安地区

Key words

Sanggan Group/rock association/zircon U-Pb dating/LA-ICP-MS/Huai'an area,Hebei

分类

天文与地球科学

引用本文复制引用

陈后华,段留安,张平阳,王卫国,宋贺民..河北怀安地区桑干岩群岩石组合特征及锆石U-Pb年代学对其形成和变质时代的约束[J].地质通报,2025,44(5):872-884,13.

基金项目

中国地质调查局项目《山东招远玲珑-水旺庄金矿资源调查评价》(编号:DD20243128) (编号:DD20243128)

地质通报

OA北大核心

1671-2552

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