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题名

Petrogenesis of Neoproterozoic magmatic rocks in the Songnen Massif (northeastern China): Implications for basement composition and crustal growth

作者
通讯作者Tang,Jie
发表日期
2022-07-15
DOI
发表期刊
ISSN
0301-9268
EISSN
1872-7433
卷号376
摘要
This paper reports new zircon U-Pb geochronological, whole-rock geochemical, and zircon Hf isotopic data for Neoproterozoic intrusive rocks in the Songnen Massif in the eastern Central Asian Orogenic Belt (CAOB), with the aim of revealing the petrogenesis of the Neopmterozoic intrusive rocks, and constraining the basement composition and crustal growth process of the Songnen Massif. Dating results identify three episodes of Neopmterozoic magmatism at ca. 950, ca. 856, and ca. 790 Ma in the eastern Songnen Massif. The ca. 950 Ma magmatic rocks consist of syenogranites, the ca. 856 Ma magmatic rocks comprise mainly gneissic monzogranites, and the ca. 790 Ma magmatic rocks consist of gneissic monzonites and monzogranites. The Neopmterozoic granitoids have high contents of SiO2 and K2O, low contents of total Fe2O3 and MgO, and show characteristics of enrichment in large-ion lithophile elements (e.g., K and Rb), and depletion in high-fieldstrength elements, implying that their primary magmas could have been derived from partial melting of the lower crust. However, compared with the ca. 790 Ma monzogranites [epsilon(Hf(t))= +7.3 to +9.5] in the south of the Songnen Massif, the ca. 950 and ca. 856 Ma granitoids in the north have much lower zircon epsilon(Hf)(t) values (-2.0 to -0.2 and -10.6 to -8.9, respectively), suggesting that the ca. 950 and ca. 856 Ma magmas were generated by the reworking of ancient mafic lower crust, whereas the ca. 790 Ma granitic magma was generated by the reworking of juvenile mafic lower crust. In contrast, the ca. 790 Ma gneissic monzonites were formed by mixing of the mantle-derived and crust-derived melts. Considering the Precambrian magmatism, detrital and captured zircons, and zircon Hf model ages together, the Precambrian basement of the Songnen Massif includes not only the Neopmterozoic crustal materials, but also the Neoarchean-Mesopmterozoic components. Zircon epsilon(Hf)(t) values of the Neoproterozoic granitoids in the Songnen Massif appear to progressively decrease from south to north, reflecting a lateral heterogeneity of basement composition of the eastern Songnen Massif, and indicating that crustal growth occurred mainly during the late Mesoproterozoic and Neoproterozoic in the south, while during the late Paleoproterozoic in the north.
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语种
英语
学校署名
其他
资助项目
National Natural Science Foundation of China["42072071","41772047"] ; Fundamental Research Funds for the Central Universities[N2123029] ; Natural Science Foundation of Hebei Province[D2020501002]
WOS研究方向
Geology
WOS类目
Geosciences, Multidisciplinary
WOS记录号
WOS:000832727400002
出版者
ESI学科分类
GEOSCIENCES
Scopus记录号
2-s2.0-85134477924
来源库
Web of Science
引用统计
被引频次[WOS]:7
成果类型期刊论文
条目标识符http://sustech.caswiz.com/handle/2SGJ60CL/359554
专题理学院_地球与空间科学系
作者单位
1.College of Earth Sciences,Jilin University,Changchun,130061,China
2.Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines,Northeastern University,Shenyang,110819,China
3.Key Laboratory of Mineral Resources Evaluation in Northeast Asia,Ministry of Land and Resources,Changchun,130061,China
4.Department of Earth and Space Science,Southern University of Science and Technology,Shenzhen,518055,China
推荐引用方式
GB/T 7714
Luan,Jin–Peng P.,Tang,Jie,Xu,Wen–Liang L.,et al. Petrogenesis of Neoproterozoic magmatic rocks in the Songnen Massif (northeastern China): Implications for basement composition and crustal growth[J]. PRECAMBRIAN RESEARCH,2022,376.
APA
Luan,Jin–Peng P.,Tang,Jie,Xu,Wen–Liang L.,Guo,Peng,Long,Xin–Yu Y.,&Xiong,Shuai.(2022).Petrogenesis of Neoproterozoic magmatic rocks in the Songnen Massif (northeastern China): Implications for basement composition and crustal growth.PRECAMBRIAN RESEARCH,376.
MLA
Luan,Jin–Peng P.,et al."Petrogenesis of Neoproterozoic magmatic rocks in the Songnen Massif (northeastern China): Implications for basement composition and crustal growth".PRECAMBRIAN RESEARCH 376(2022).
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