Genesis and tectonic setting of Cuiluan plutonic complex in the south section of the Xiaoxing'an Mountains: Evidences of geochemical and zircon Hf isotope

YANG Yuanjiang; ZHANG Lidong; YANG Wenpeng; LI Chenglu; GUO Fenglei; ZHAO Handong; DENG Changzhou; SHEN Long; SHEN Liang

doi:10.12097/gbc.2022.09.019

2024 Vol. 43, No. 2~3

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Article navigation > Geological Bulletin of China > 2024 > 43(2~3): 416-428

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YANG Yuanjiang, ZHANG Lidong, YANG Wenpeng, LI Chenglu, GUO Fenglei, ZHAO Handong, DENG Changzhou, SHEN Long, SHEN Liang. 2024. Genesis and tectonic setting of Cuiluan plutonic complex in the south section of the Xiaoxing'an Mountains: Evidences of geochemical and zircon Hf isotope. Geological Bulletin of China, 43(2~3): 416-428. doi: 10.12097/gbc.2022.09.019

Citation:

YANG Yuanjiang, ZHANG Lidong, YANG Wenpeng, LI Chenglu, GUO Fenglei, ZHAO Handong, DENG Changzhou, SHEN Long, SHEN Liang. 2024. Genesis and tectonic setting of Cuiluan plutonic complex in the south section of the Xiaoxing'an Mountains: Evidences of geochemical and zircon Hf isotope. Geological Bulletin of China, 43(2~3): 416-428. doi: 10.12097/gbc.2022.09.019

Genesis and tectonic setting of Cuiluan plutonic complex in the south section of the Xiaoxing'an Mountains: Evidences of geochemical and zircon Hf isotope

1.
Heilongjiang Institute of Natural Resources Survey, Harbin 150036, Heilongjiang, China
2.
The First Institute of Geological Exploration of Heilongjiang Province, Mudanjiang 157011, Heilongjiang, China
3.
Institute of Geochemistry Chinese Academy of Sciences, Guiyang 550081, Guizhou, China
4.
Development and Research Center, China Geology Survey, Beijing 100037, China

More Information

Corresponding author: SHEN Liang, 2547163401@qq.com

Received Date: 21 September 2022

Revised Date: 27 February 2023

Publish Date: 15 March 2024

Abstract

Abstract

This paper studies the chronology, rock geochemistry and zircon Hf isotopic characteristics of the Middle Ordovician Cuiluan plutonic complex in the south section of the Xiaoxing'an Mountains in Heilongjiang Province, focusing on the formation age, petrogenesis, magmatic material source and tectonic background of the rock mass. Using laser ablation plasma mass spectrometer (LA−ICP-MS) zircon U−Pb dating method, the ages of granodiorite and granite porphyry samples are dated to be 463±2 Ma and 462±2 Ma, i.e., Middle Ordovician. The study of rock geochemistry shows that both samples are characterized by high Si and K, rich alkali, and poor Ti, Mg, Fe, P, etc. It is enriched in LILE (e.g., Rb, K ), depleted in HFSE (e.g., Ti, Nb, Ta, P and HREE) with significant negative Eu anomalies（δ Eu= 0.38~0.64), which show the crust source characteristics of magma. Zircon ε_Hf (t)=2.4~3.4, the values are concentrated and distributed above the chondrite line, indicating that the magma source area is the partial melting of the new continental crust material. T_DM^c = 1128~1070 Ma, confirming the existence of Mesoproterozoic crustal accretion events in this area. This study suggests that the Cuiluan complex was formed in the tectonic environment of subduction of oceanic and continental plates.
- plutonic complex /
- zircon U−Pb ages /
- zircon Hf isotope /
- petrogenesis /
- South of Xiaoxing'an Mountains

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