首页|浙西北钟吕群流纹岩锆石U-Pb年龄及其年代地层学意义

浙西北钟吕群流纹岩锆石U-Pb年龄及其年代地层学意义

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钟吕群出露于浙西北地区,为一套强变形、浅变质的碎屑岩—火山岩系,其下未见底,上被南华纪休宁组不整合覆盖.传统上将其对比于赣东北双桥山群.本文主要研究钟吕群流纹岩的锆石U-Pb年龄.样品A120408-4采自苏庄断层以北,层位上属钟吕群的中上部,岩性为灰白色致密块状流纹岩,强烈片理化.样品A120408-4中获得大量锆石,完成LA-ICP-MS锆石U-Pb定年测点38个,获得年龄加权平均值为(777.1±3.6) Ma,结合地层特点及变质变形特征,得出钟吕群主体相当于河上镇群上墅组,应属扬子古陆新元古代晚期大陆裂谷的地质记录.
LA-ICP-MS zircon U-Pb dating of the rhyolite from the Zhonglü Group,northwestern Zhejiang Province, and its chronostratigraphic significance
The Zhonglü Group,outcropped in the northwestern part of Zhejiang Province,is a sequence of strongly-deformed,low-grade metamorphic clastic and volcanic rocks.It is overlaid unconformably by the Xiuning Formation,Nanhua period.Traditionally it is compared to the Shuangqiaoshan Group in the northeastern part of Jiangxi Province.This paper reports the LA-ICP-MS zircon U-Pb age of the rhyolite from the Zhonglüi Group.The age of the Zhonglü Group is important to remodeling stratigraphic classification and correlation of Precambrian,and the mineralization geological background and conditions in the east part of South China are important as well.Sample A120408-4,collected from the north of Suzhuang fault,the middle-upper part of the Zhonglü Group,is massive rhyolite,which had been heavily foliated.Thirty-eight of the zircons were analyzed with LA-ICP-MS,and a weighed-mean U-Pb age of (777.1 ± 3.6) Ma was obtained.Considering the stratum and metamorphic deformation characteristics,we draw the following conclusion:The main part of the Zhonglüi Group is equivalent to the Shangshu Formation,Heshangzhen Group.Both of them belong to different facies of the same period,and they developed under the global tectonic background of Rodinia supercontinent cracking.The Zhonglü Group represents the cracking of the Yangtze ancient continent in the late neoproterozoic.

Zhonglü GroupShangshu FormationLA-ICP-MSzircon U-Pb agerhyoliteneoproterozoic

韩瑶、张传恒、蒋先强、游国庆、刘子荟

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中国地质大学(北京)地球科学与资源学院,北京100083

中国地质科学院成都矿产综合利用研究所,成都610041

中国地质科学院地质研究所,北京100037

钟吕群 上墅组 LA-ICP-MS 锆石U-Pb 流纹岩 新元古代

中国地质调查局项目国家自然科学基金国家科技重大专项

121201112011740921062AB1201

2016

科技导报
中国科学技术协会

科技导报

CSTPCDCSCD北大核心
影响因子:0.559
ISSN:1000-7857
年,卷(期):2016.34(2)
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