必须声明标量变量 "@Script_ID"。 大别山造山带宿松岩群锆石U-Pb年龄和Nd同位素特征:宿松地体物源和属性-《地球科学与环境学报》
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[1]李俊辉,于洋,韦龙猛,等.大别山造山带宿松岩群锆石U-Pb年龄和Nd同位素特征:宿松地体物源和属性[J].地球科学与环境学报,2016,38(01):21-33.
 LI Jun-hui,YU Yang,WEI Long-meng,et al.Zircon U-Pb Ages and Nd Isotopic Characteristics of Susong Group in Dabie Orogenic Belt: Source and Provenance of Susong Terrene[J].Journal of Earth Sciences and Environment,2016,38(01):21-33.
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大别山造山带宿松岩群锆石U-Pb年龄和Nd同位素特征:宿松地体物源和属性(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第38卷
期数:
2016年第01期
页码:
21-33
栏目:
基础地质与矿产地质
出版日期:
2016-01-15

文章信息/Info

Title:
Zircon U-Pb Ages and Nd Isotopic Characteristics of Susong Group in Dabie Orogenic Belt: Source and Provenance of Susong Terrene
文章编号:
1672-6561(2016)01-0021-13
作者:
李俊辉于洋韦龙猛胡昭平陈福坤
中国科学技术大学 地球和空间科学学院,安徽 合肥 230026
Author(s):
LI Jun-hui YU Yang WEI Long-meng HU Zhao-ping CHEN Fu-kun
School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, Anhui, China
关键词:
地壳演化构造属性前寒武纪U-Pb年龄Nd同位素宿松岩群扬子陆块大别造山带
Keywords:
crustal evolution structure provenance Precambrian U-Pb age Nd isotope Susong Group Yangtze Block Dabie orogen belt
分类号:
P597
DOI:
-
文献标志码:
A
摘要:
大别超高压变质造山带南部的宿松地体主要由高压变质宿松岩群或杂岩组成,其岩性和物源构成复杂,历来的研究颇具争议。报道了宿松岩群的片麻岩、片岩和变质基性岩石等主要岩石类型的锆石U-Pb年龄和Nd 同位素组成,限定了岩石地球化学特征,探讨了宿松地体的属性及地壳演化。两个片麻岩样品的锆石U-Pb同位素年龄为750 Ma至约770 Ma,初始εNd值为-7.3~-1.6,可以推测原岩为新元古代岩浆岩;两个片岩样品的碎屑锆石U-Pb年龄值分布范围较大,并主要集中于晚太古代(2 700 Ma至约2 800 Ma)、早元古代(2 000 Ma至约2 500 Ma)、中元古代(1 100 Ma至约1 500 Ma)和新元古代(700 Ma至约800 Ma),推测原岩为新元古代沉积岩。片岩的Nd同位素组成变化较大,初始εNd值(回扣至750 Ma)为-20.2~-1.4,暗示剥蚀区的物质组成复杂。相似的碎屑锆石U-Pb年龄分布特征也普遍地记录在扬子陆块的基底岩石或沉积盖层中。新元古代岩浆岩广泛分布于宿松岩群、大别—苏鲁造山带超高压变质地体乃至扬子陆块边缘,指示宿松高压变质地体具有扬子陆块属性和相似的地壳演化历史。
Abstract:
Susong Group or Susong rock complex is the major rock unit of Susong terrene in the southern part of Dabie ultrahigh-pressure orogenic belt. Rocks of this group undergo high-pressure metamorphism and have complex origins or sources, and hence, the provenance and evolution history of Susong terrene are still debated. Zircon U-Pb ages and whole-rock Nd isotopic data for gneisses, schists and metabasic rocks of Susong Group were presented to place geochemical characteristics of Susong Group, and the evolution of the crust and provenance of Susong terrene were discussed. Zircons separated from two gneiss samples yield U-Pb ages of 750 to ~770 Ma, suggesting as evidence for a magmatic event in Neoproterozoic. Initial εNd values of whole-rocks of the gneisses range from -7.3 to -1.6. Detrital zircons from two schist samples give a wide range of U-Pb ages, clustering around Late Archean (2 700 Ma to ~2 800 Ma), Paleoproterozoic (2 000 Ma to ~2 500 Ma), Mesoproterozoic (1 100 Ma to ~1 500 Ma) and Neoproterozoic (700 to ~800 Ma), implying Neoproterozoic sedimentary rocks as their protoliths. Initial εNd values of whole-rocks of the schists vary from -20.2 to -1.4, when calculated back to 750 Ma, suggesting complex rock components in the source area. Similar distribution patterns of detrital zircon U-Pb ages are also commonly recorded in the basement or sedimentary cover rocks exposed in Yangtze Block. The Neoproterozoic magmatic rocks are widely distributed in Susong Group, ultrahigh-pressure metamorphic terrenes of Dabie-Sulu orogenic belt and the continental margins of Yangtze Block, indicating that Susong high-pressure metamorphic terrene is of a Yangtze affinity and has had similar history of the crustal evolution.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2015-08-02
基金项目:国家自然科学基金项目(40973042,41090372)
作者简介:李俊辉(1990-),男,安徽宿州人,理学硕士研究生,E-mail:phila3lee@gmail.com。
通讯作者:陈福坤(1964-),男,福建龙海人,教授,博士研究生导师,理学博士,E-mail:fkchen@ustc.edu.cn。
更新日期/Last Update: 2016-01-30