中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochronology and geochemistry of Early Cretaceous high-silica granites in the Nan'ao Island, South China: Petrogenesis and implications for lithospheric extension

文献类型:期刊论文

作者Zhou, Dawn; Sun, Peng; Jiang, Shijun; Liu, Xiao; Wang, Qiang
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2023
卷号245页码:105558
关键词A-TYPE GRANITES CRUST-MANTLE INTERACTION GAN-HANG BELT U-PB AGE SOUTHEASTERN CHINA TECTONIC SIGNIFICANCE ISOTOPIC CONSTRAINTS VOLCANIC-ROCKS TRACE-ELEMENTS COASTAL AREA
ISSN号1367-9120
DOI10.1016/j.jseaes.2023.105558
英文摘要Widespread Late Mesozoic granites in South China are known to be younger southeastward, which is important for understanding the tectonic-magmatic evolution in South China. However, previous studies assumed Jurassic or Late Cretaceous ages for some granites in the Nan'ao Island, contradicting with the established trend. To address such controversy, we have carried out geochronological and geochemical studies of several granite plutons in this island. New zircon U-Pb age data show that they were emplaced in the Early Cretaceous from similar to 141 Ma in the Dajianshan area to 123-121 Ma in the Forest Park and Hulu-Guolaoshan areas, confirming that the southeastward younger trend of granitic magmatism had reached Nan'ao Island. These granites are characterized by high SiO2 (74.2-77.8 wt%) and low Al2O3 (12.0-13.1 wt%) contents, pronounced negative Ba-Eu-Sr-Ti anomalies, and moderately high temperatures of magmas (T-Zr = 655-771 degrees C; T-LREE = 675-819 degrees C). The Dajianshan granites have lower epsilon(Nd)(t) (-3.9 to -3.6), Nb/Ta (6.8-12), and Zr/Hf (16-22) than the Forest Park and Hulu-Guolaoshan granites (-1.5 to + 1.1, 9.4-16, and 20-30). The new data support the interpretation that the parental magmas for the Dajianshan granites were derived from a mixture of juvenile crustal rocks and Proterozoic metamorphic rocks whereas the parental magmas for the Forest Park and Hulu-Guolaoshan granites were sourced from juvenile crustal rocks. We envision that partial melting in the crust was induced by under -plating of mantle-derived mafic magma, which in turn was produced by decompression melting of ascending asthenospheric mantle in response to rollback of the subducting Paleo-Pacific plate.
WOS研究方向Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000927306600001
源URL[http://ir.gig.ac.cn/handle/344008/80388]  
专题同位素地球化学国家重点实验室
推荐引用方式
GB/T 7714
Zhou, Dawn,Sun, Peng,Jiang, Shijun,et al. Geochronology and geochemistry of Early Cretaceous high-silica granites in the Nan'ao Island, South China: Petrogenesis and implications for lithospheric extension[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,245:105558.
APA Zhou, Dawn,Sun, Peng,Jiang, Shijun,Liu, Xiao,&Wang, Qiang.(2023).Geochronology and geochemistry of Early Cretaceous high-silica granites in the Nan'ao Island, South China: Petrogenesis and implications for lithospheric extension.JOURNAL OF ASIAN EARTH SCIENCES,245,105558.
MLA Zhou, Dawn,et al."Geochronology and geochemistry of Early Cretaceous high-silica granites in the Nan'ao Island, South China: Petrogenesis and implications for lithospheric extension".JOURNAL OF ASIAN EARTH SCIENCES 245(2023):105558.

入库方式: OAI收割

来源:广州地球化学研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。