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Petrogenesis of Jurassic granitoids at the northeastern margin of the North China Craton: New geochemical and geochronological constraints on subduction of the Paleo-Pacific Plate

Published on Jun 1, 2018in Journal of Asian Earth Sciences2.76
· DOI :10.1016/j.jseaes.2018.03.006
Jin Liu4
Estimated H-index: 4
(SYSU: Sun Yat-sen University),
Jian Zhang5
Estimated H-index: 5
(SYSU: Sun Yat-sen University)
+ 3 AuthorsYoubo Peng2
Estimated H-index: 2
Abstract
Abstract At the junction between the North China Craton (NCC) and the Central Asian Orogenic Belt (CAOB), northern Liaoning province, NE China, there are widespread Jurassic igneous rocks. The tectonic setting and petrogenesis of these rocks are unresolved. Zircon U–Pb dating, whole-rock geochemistry, and Hf isotopic compositions of Jurassic granitoids were investigated to constrain their ages and petrogenesis in order to understand the tectonic evolution of the Paleo-Pacific Ocean along the northeastern margin of the NCC. Geochronological data indicate that magmatism occurred between the early and late Jurassic (180–156 Ma). Despite the wide range in ages of the intrusions, Jurassic granitoids were likely derived from a similar or common source, as inferred from their geochemical and Hf isotopic characteristics. Compared to the island arc andesite-dacite-rhyolite series, the Jurassic granitoids are characterized by higher SiO 2 , Al 2 O 3 , and Sr contents, and lower MgO, FeO T , Y, and Yb contents, indicating that the primary magmas show typical characteristics of adakitic magmas derived from partial melting of thickened lower crust. These findings, combined with their e Hf (t) values (+1.4 to +5.4) and two-stage model ages (1515–1165 Ma), indicate the primary magmas originated from partial melting of juvenile crustal material accreted during the Mesoproterozoic. They are enriched in large-ion lithophile elements (e.g., Rb, K, Th, Ba, and U) and light rare-earth elements (REE), and depleted in high-field-strength elements (e.g., Nb, Ta, Ti, and P) and heavy REE. Based on these findings and previous studies, we suggest that the Jurassic adakitic granitoids (180–156 Ma) were formed in an active continental margin and compressive tectonic setting, related to subduction of the Paleo-Pacific Plate.
  • References (83)
  • Citations (5)
References83
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#2Neng Jiang (CAS: Chinese Academy of Sciences)H-Index: 20
Last.Keqing Zong (China University of Geosciences)H-Index: 27
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#1Shan Li (NTU: National Taiwan University)H-Index: 10
#2Sun-Lin Chung (NTU: National Taiwan University)H-Index: 66
Last.Qianqian Guo (CAS: Chinese Academy of Sciences)H-Index: 12
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#1Xiao-Yao Zhou (CAS: Chinese Academy of Sciences)H-Index: 4
#2Xin Jin (CAS: Chinese Academy of Sciences)H-Index: 5
Last.Yu-Xiu Zhang (CAS: Chinese Academy of Sciences)H-Index: 16
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Cited By5
Newest
#1Zuozhen Han (SDUST: Shandong University of Science and Technology)H-Index: 17
#2Xiang Ren (SDUST: Shandong University of Science and Technology)H-Index: 1
Last.Lihua Gao (SDUST: Shandong University of Science and Technology)H-Index: 6
view all 9 authors...
#1Jia-Lin Cao (JLU: Jilin University)H-Index: 5
#2Jian-Bo Zhou (JLU: Jilin University)H-Index: 25
Last.Long Li (U of A: University of Alberta)H-Index: 15
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