Geochronology and geochemistry of granites in Linhai forest farm, northern Xiaoxinganling Mountains: Tectonic implication

MU Fu-quan; XU Guo-yu; LU Hong-yan; CUI Xue-wen; CHANG Liang; LOU Yu-lei; QI Ying-sheng; QIU Xin-dong

doi:10.13686/j.cnki.dzyzy.2025.01.001

2025 Vol. 34, No. 1

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Article navigation > Geology and Resources > 2025 > 34(1): 1-10, 102

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MU Fu-quan, XU Guo-yu, LU Hong-yan, CUI Xue-wen, CHANG Liang, LOU Yu-lei, QI Ying-sheng, QIU Xin-dong. Geochronology and geochemistry of granites in Linhai forest farm, northern Xiaoxinganling Mountains: Tectonic implication[J]. Geology and Resources, 2025, 34(1): 1-10, 102. doi: 10.13686/j.cnki.dzyzy.2025.01.001

Citation:

MU Fu-quan, XU Guo-yu, LU Hong-yan, CUI Xue-wen, CHANG Liang, LOU Yu-lei, QI Ying-sheng, QIU Xin-dong. Geochronology and geochemistry of granites in Linhai forest farm, northern Xiaoxinganling Mountains: Tectonic implication[J]. Geology and Resources, 2025, 34(1): 1-10, 102. doi: 10.13686/j.cnki.dzyzy.2025.01.001

Geochronology and geochemistry of granites in Linhai forest farm, northern Xiaoxinganling Mountains: Tectonic implication

1.
Mudanjiang Natural Resources Comprehensive Survey Center, Mudanjiang 157021, Heilongjiang Province, China
2.
Liaoning Natural Resources Affairs Service Center, Shenyang 110033, China

More Information

Corresponding author: XU Guo-yu, xuguoyu@mail.cgs.gov.cn

Received Date: 10 July 2023

Revised Date: 16 October 2023

Publish Date: 25 February 2025

Abstract

Abstract

A series of highly fractionated Ⅰ-type granites, mainly composed of marginal facies fine-grained monzogranite and central facies fine-medium-grained monzogranite, is developed in Linhai forest farm area of the Xiaoxinganling-Zhangguangcailing mountains. The granites are characterized by high Si and total alkali (Na₂O+K₂O), rich Al, and poor Fe, Mg, Ca and Ti, belonging to quasi-aluminous, high-K calc-alkaline series, with enriched LILEs and LREEs, depleted HFSEs, and moderately strong negative Eu anomaly. The LA-ICP-MS zircon U-Pb age results show that the granites were formed at 191.6±2.9 Ma. According to the geochemical compositions, it is considered that the granites are mainly derived from the partial melting of shallow continental crust materials in Early Mesozoic. The discovery of highly fractionated Ⅰ-type granites indicates that large-scale magmatic intrusion occurred in the Early Jurassic, which may be closely related to the regional extensional environment under the westward subduction of paleo-Pacific plate.
- Early Jurassic /
- granite /
- geochronology /
- geochemistry /
- tectonic setting /
- Xiaoxinganling /
- Zhangguangcailing

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References

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