腾冲地区新生代高钾钙碱性火山岩结构组成及形成过程

江涛; 郑建平; 苏玉平; 杨志国; 李鑫

doi:10.3799/dqkx.2025.173

Volume 50 Issue 11

Nov. 2025

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Jiang Tao, Zheng Jianping, Su Yuping, Yang Zhiguo, Li Xin, 2025. Structure Composition and Formation Process of Cenozoic High-K Calc-Alkaline Volcanic Rocks in Tengchong Area. Earth Science, 50(11): 4387-4404. doi: 10.3799/dqkx.2025.173

Citation:

Jiang Tao, Zheng Jianping, Su Yuping, Yang Zhiguo, Li Xin, 2025. Structure Composition and Formation Process of Cenozoic High-K Calc-Alkaline Volcanic Rocks in Tengchong Area. Earth Science, 50(11): 4387-4404. doi: 10.3799/dqkx.2025.173

Citation:

Jiang Tao, Zheng Jianping, Su Yuping, Yang Zhiguo, Li Xin, 2025. Structure Composition and Formation Process of Cenozoic High-K Calc-Alkaline Volcanic Rocks in Tengchong Area. Earth Science, 50(11): 4387-4404. doi: 10.3799/dqkx.2025.173

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Structure Composition and Formation Process of Cenozoic High-K Calc-Alkaline Volcanic Rocks in Tengchong Area

doi: 10.3799/dqkx.2025.173

Jiang Tao^{1, 2
,
,},
Zheng Jianping^{2
,
,},
Su Yuping^{1, 2},
Yang Zhiguo¹,
Li Xin³

1.
Key Laboratory of Green and Intelligent Development and Efficient Utilization of Strategic Mineral Resources of Xinjiang Production and Construction Corps, School of Natural Resources Science and Technology, Xinjiang University of Technology, Hotan 848000, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
3.
Hotan Geological Brigade of Xinjiang Uygur Autonomous Region Geological Bureau, Hotan 848000, China

Received Date: 2025-05-06
Publish Date: 2025-11-25

Abstract

Abstract

Since the Cenozoic, a large amount of high-potassium calc-alkaline volcanic rocks (basaltic trachyandesite and trachyandesite) have developed in the Tengchong area, but the specific formation process remains unclear. Based on petrographic analysis, in this paper it conducts whole-rock major element and mineral major and trace element analyses of these volcanic rocks, and discusses their formation and evolution process in combination with the published data. The rocks commonly exhibit porphyritic textures, with phenocrysts predominantly consisting of olivine, pyroxene, and plagioclase, and the development of glomerocrysts. Clinopyroxene phenocrysts commonly show normal zoning, reverse zoning, and oscillatory zoning, with oscillatory zoning indicating multi-stage mafic magma replenishment and possible local contamination during magma evolution. Whole-rock major element analysis reveals that these rocks belong to the high-potassium calc-alkaline rock series. Clinopyroxene, orthopyroxene, and plagioclase phenocrysts and glomerocrysts show similar REE and trace element distribution patterns, with clinopyroxene being the most enriched in trace elements, followed by plagioclase, and orthopyroxene showing the lowest concentrations. The geochemical characteristics of olivine phenocrysts suggest that the magma source region may have originated from partial melting of peridotite, while the trace element compositions of the whole rocks and clinopyroxene phenocrysts record geochemical signatures characteristic of an arc-related tectonic setting. The mineral equilibrium temperature-pressure calculations reveal the existence of two intermediate to felsic magma reservoirs beneath the study area: a shallow dacitic magma reservoir (depth 8.3-13.6 km) and a deep andesitic magma reservoir (depth 18.4-30.2 km). The studied samples are derived from the deeper reservoir. Their formation involves mafic magma recharge, triggering mixing between crystal mush and melt; when newly generated melts become dominant within the reservoir, eruption is triggered, carrying semi-consolidated magmatic clots to the surface and forming the typical (glomerocrystic) textures.
- Cenozoic,
- high-K calc-alkaline volcanic rocks,
- phenocryst,
- magma reservoir,
- Tengchong area,
- rare earth elements,
- petrology

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References(89)

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Structure Composition and Formation Process of Cenozoic High-K Calc-Alkaline Volcanic Rocks in Tengchong Area

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