Geochronology and geochemistry of Haliheiba pluton in the central and southern Great Hinggan Range and its tectonic delamination

WEI Wei; HUANG Xingkai; XU Qiao; JIANG Binbin; LIU Zi; ZHU Xinyou; WU Xiyong

doi:10.12029/gc20200706001

2024 Vol. 51, No. 3

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WEI Wei, HUANG Xingkai, XU Qiao, JIANG Binbin, LIU Zi, ZHU Xinyou, WU Xiyong. 2024. Geochronology and geochemistry of Haliheiba pluton in the central and southern Great Hinggan Range and its tectonic delamination[J]. Geology in China, 51(3): 978-994. doi: 10.12029/gc20200706001

Citation:

WEI Wei, HUANG Xingkai, XU Qiao, JIANG Binbin, LIU Zi, ZHU Xinyou, WU Xiyong. 2024. Geochronology and geochemistry of Haliheiba pluton in the central and southern Great Hinggan Range and its tectonic delamination[J]. Geology in China, 51(3): 978-994. doi: 10.12029/gc20200706001

Geochronology and geochemistry of Haliheiba pluton in the central and southern Great Hinggan Range and its tectonic delamination

1.
School of Civil Engineering, Southwest Jiaotong University, Chengdu 610031, Sichuan, China
2.
Faculty of Geosciences and Engineering, Southwest Jiaotong University, Chengdu 611756, Sichuan, China
3.
Zijin Mining Group Co. Ltd., Shanghang 364200, Fujian, China
4.
Bejing Eco–friendly Exploration Technology Co. Ltd., Beijing 101100, China
5.
Sino–Zijin Resources, Beijing 100012, China
6.
Beijing Institute of Geology for Mineral Resources Co. Ltd., Beijing 100012, China

Fund Project: Supported by the project of China Geological Survey (No.DD20160072).

More Information

Author Bio: WEI Wei, male, born in 1993, doctor, engaged in prediction and assessment of mineral resources; E-mail: lamborww0801@sina.com

Received Date: 06 July 2020

Revised Date: 27 August 2020

Publish Date: 25 May 2024

Abstract

Abstract

This paper is the result of geological survey engineering.
Objective
The diagenetic age, petrogenetic types, source properties and geodynamic background of the Early Cretaceous granites of Haliheba pluton in the central and southern part of Great Hinggan Range are discussed based on the regional geological survey.
Methods
The lithography of granite, U–Pb chronology, geochemistry and Hf isotope composition of zircon are studied by means of microscope, XRF and (LA–) ICP–MS.
Results
The Early Cretaceous granites in Haliheiba are composed of fine to medium–grained biotite granite and fine–grained porphyritic biotite granite, and zircon U–Pb ages are (139.1±0.7) Ma and (138.4±1.0) Ma, respectively. The granites are characterized by high SiO₂ (74.09%−77.19%) and alkali enrichment (7.92%−8.46%), and belong to high–K calc–alkaline series. The A/CNK values range from 0.95 to 1.08, indicating that they are metaluminous to weakly peraluminous rocks. The chrondrite–normalized REE patterns are characterized by enrichment of LREEs with (La/Yb)_N values varying from 3.69 to 13.17 and by prominent negative Eu anomalies with δEu values ranging from 0.11 to 0.47. The granites show the enrichment of Rb, U, Th , Nb, Ta, Zr and Hf, and the depletion of Sr, Ba, Ti and P. Zircon Hf isotopic compositions suggest that these granites have high positive ε_Hf(t) values (+5.0 − +11.2) and fairly young two–stage Hf model ages (408−731 Ma).
Conclusions
The Haliheiba granites are aluminous A–type granites, which were mainly derived from partial melting of the juvenile crustal materials associated with ancient crustal materials under extensional tectonic setting that was probably controlled by lithospheric delamination and thinning.
- zircon U–Pb chronology /
- Early Cretaceous granite /
- Hf isotope /
- Haliheiba /
- central and southern Great Hinggan Range /
- geological survey engineering

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