Extraction of high-silica granites from an upper crustal magma reservoir: Insights from the Narusongduo magmatic system, Gangdese arc
Abstract
The genesis of high-silica igneous rocks is important for understanding the behavior of shallow magmatic systems. However, although many such studies have focused on the eruption of crystal-poor high-SiO2 rhyolites, the origin of high-silica granites (HSGs) has received comparatively little attention. Here, we present a detailed study of HSGs from the Narusongduo volcanic complex, Gangdese arc. Combining zircon U-Pb geochronology with stratigraphic investigations, we show that the Narusongduo magmatic system was constructed over a period of ≥3.7 Myr with or without lulls. On the basis of zircon textures and ages, diverse zircon populations, including antecrysts and autocrysts, are recognized within the HSGs and volcanic rocks. All of the igneous rocks within the Narusongduo volcanic complex have highly radiogenic Sr–Nd isotopic compositions. Our results indicate the presence of an andesitic magma reservoir in the upper crust at a paleodepth of ~8 km. Ubiquitous zircon antecrysts in the HSGs, combined with compositional similarities between the HSGs and evolved melts of the andesitic magma reservoir, indicate that the Narusongduo HSGs represent melts extracted from the shallow magma reservoir. In addition, our results suggest that magma recharge promoted the escape of high-silica melts to form the Narusongduo HSGs. This work presents an excellent case that kilometer-scale high-silica granites are the differentiated products from an upper crustal magma reservoir. It would make a contribution to contemporary debates concerning the efficiency of crystal–melt separation in upper crustal magmatic systems.
Funding source: National Natural Science Foundation
Award Identifier / Grant number: 91855215
Award Identifier / Grant number: 41630208
Award Identifier / Grant number: 41802061
Funding source: Chinese Academy of Sciences
Award Identifier / Grant number: XDA2007030402
Award Identifier / Grant number: GIGCAS 135
Award Identifier / Grant number: 135TP201601
Funding statement: This research was supported in part by the National Key Research and Development Program of China “Deep Structure and Ore-forming Process of Main Mineralization System in Tibetan Orogen” (2016YFC0600306) to Z. S. Yang; the Second Tibetan Plateau Scientific Expedition and Research (STEP) (2019QZKK0702), the National Natural Science Foundation of China (91855215 and 41630208), the Strategic Priority Research Program (A) of the Chinese Academy of Sciences (grant no. XDA2007030402), and the Guangzhou Institute of Geochemistry, Chinese Academy of Science (GIGCAS 135 project (135TP201601) to Q. Wang; the National Natural Science Foundation of China (41802061) to J.S. Zhou.
Acknowledgments
We thank Gareth Fabbro for discussions on equilibrium liquid calculation and Mg diffusion in plagioclase. We appreciate Ya-Nan Yang, Qing Yang, Le Zhang, Peng-Li He, Fan Yang, and Peng-Fei Ma for laboratory assistance, as well as Ying-Chao Liu, Zhen-Qing Li, Qi-Wei Li, Tong-Yu Huang, Xiao-Yan Zhao, Fan Fei, Xiong Zhang, and Yu-Tao Xu for extensive help on geologic mapping and stratigraphic investigation in the field. We are grateful to Calvin Barnes, Erik Klemetti, and an anonymous reviewer for helpful, constructive reviews and Chad Deering for comments on early versions.
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Artikel in diesem Heft
- Roebling Medal Paper
- The effects of solid-solid phase equilibria on the oxygen fugacity of the upper mantle
- Structural and spectroscopic study of the kieserite-dwornikite solid-solution series, (Mg,Ni)SO4·H2O, at ambient and low temperatures, with cosmochemical implications for icy moons and Mars
- Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc
- An evolutionary system of mineralogy. Part II: Interstellar and solar nebula primary condensation mineralogy (>4.565 Ga)
- Swelling capacity of mixed talc-like/stevensite layers in white/green clay infillings (“deweylite”/“garnierite”) from serpentine veins of faulted peridotites, New Caledonia
- Experimental observations of TiO2 activity in rutile-undersaturated melts
- Direct evidence for the source of uranium in the Baiyanghe deposit from accessory mineral alteration in the Yangzhuang granite porphyry, Xinjiang Province, northwest China
- Extraction of high-silica granites from an upper crustal magma reservoir: Insights from the Narusongduo magmatic system, Gangdese arc
- “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” byAngel et al. (2017)—Discussion
- “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” —Reply to Zhong et al
- Letter
- Synthesis and crystal structure of Pb-dominant tourmaline
- Element loss to platinum capsules in high-temperature–pressure experiments
- New Mineral Names
- Book Review
- Book Review: Fundamental Planetary Science: Physics, Chemistry and Habitability
Artikel in diesem Heft
- Roebling Medal Paper
- The effects of solid-solid phase equilibria on the oxygen fugacity of the upper mantle
- Structural and spectroscopic study of the kieserite-dwornikite solid-solution series, (Mg,Ni)SO4·H2O, at ambient and low temperatures, with cosmochemical implications for icy moons and Mars
- Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc
- An evolutionary system of mineralogy. Part II: Interstellar and solar nebula primary condensation mineralogy (>4.565 Ga)
- Swelling capacity of mixed talc-like/stevensite layers in white/green clay infillings (“deweylite”/“garnierite”) from serpentine veins of faulted peridotites, New Caledonia
- Experimental observations of TiO2 activity in rutile-undersaturated melts
- Direct evidence for the source of uranium in the Baiyanghe deposit from accessory mineral alteration in the Yangzhuang granite porphyry, Xinjiang Province, northwest China
- Extraction of high-silica granites from an upper crustal magma reservoir: Insights from the Narusongduo magmatic system, Gangdese arc
- “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” byAngel et al. (2017)—Discussion
- “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” —Reply to Zhong et al
- Letter
- Synthesis and crystal structure of Pb-dominant tourmaline
- Element loss to platinum capsules in high-temperature–pressure experiments
- New Mineral Names
- Book Review
- Book Review: Fundamental Planetary Science: Physics, Chemistry and Habitability