Zircon geochronological and geochemical insights into pluton building and volcanic-hypabyssal-plutonic connections: Oki-Dōzen, Sea of Japan—A complex intraplate alkaline volcano
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Jane H. Scarrow
Abstract
The relationship between plutonic and volcanic components of magmatic plumbing systems continues to be a question of intense debate. The Oki-Dōzen Islands, Sea of Japan, preserve outcrops of temporally associated plutonic, hypabyssal, and volcanic rocks. Post-intrusion uplift juxtaposed Miocene syenites in inferred faulted contact with volcanic trachytes that are cut by rhyolite hypabyssal dikes. This provides a window deep into the timing and origins of magma storage architecture and dynamics. Zircon is ubiquitous in all samples; our aim is to determine what its age and composition can reveal about the plutonic-volcanic connection. Here we show magma source characteristics are recorded in zircon Hf isotopes; source composition and assimilation of heterogeneous hydrothermally altered crust in zircon O isotopes; and extensive fractional crystallization in zircon trace elements. Combined with new U-Th-Pb SHRIMP zircon ages, 6.4–5.7 Ma, compositional data show pluton formation was by protracted amalgamation of discrete magma pulses. The rhyolite dike preserves an evolved fraction segregated from these discrete magmas. Synchronous with plutonism was a volcanic eruption of trachyte magma derived from the same source, which may have stalled at a relatively shallow depth prior to eruption. Stalling occurred at least above the amphibole stability zone because amphibole-compatible Sc and Ti were not depleted in the trachyte melt resulting in elevated values of these in volcanic compared to plutonic zircon. Identifying smaller episodic magma pulses in a larger magmatic complex places constraints on potential magma fluxes and eruptible volumes. High-flux, large volume, plume-related ocean island magmatic systems may have extensive vertically distributed multi-stage magmatic reservoirs and subduction-related systems transcrustal magma reservoirs. By contrast, Oki-Dōzen was a low-flux system with incremental pluton growth and small- to moderate-scale eruptions.
Funding statement: Data collection for this project has received funding from the European Union’s Horizon 2020 research and innovation program under the Marie Skłodowska-Curie grant agreement no. 749611 (J.H.S.) and Japan Society for the Promotion of Science postdoctoral fellowship no. PE16724 (K.J.C.). We also acknowledge funding from the Spanish grant CGL2017-84469-P. This is the IBERSIMS publication no. 87.
Acknowledgments
We are grateful to T. Sato (JAMSTEC), R. Senda (Kyushu University), and G. Cooper (Cardiff University) for technical assistance and valuable discussions. Callum Hetherington is thanked for editorial handling and detailed comments that significantly improved the manuscript. We are much obliged to reviewers Marco Brenna and John Encarnacion for the time and effort they took to help us improve the clarity and rigor of our interpretations.
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Artikel in diesem Heft
- Estimating kaolinite crystallinity using near-infrared spectroscopy: Implications for its geology on Earth and Mars
- The interplay between twinning and cation inversion in MgAl2O4-spinel: Implications for a nebular thermochronometer
- The effect of fluorine on reaction-rim growth dynamics in the ternary CaO-MgO-SiO2 system
- Seeing through metamorphic overprints in Archean granulites: Combined high-resolution thermometry and phase equilibrium modeling of the Lewisian Complex, Scotland
- Interphase misorientation as a tool to study metamorphic reactions and crystallization in geological materials
- Trace element partitioning between olivine and melt in lunar basalts
- Solving the iron quantification problem in low-kV EPMA: An essential step toward improved analytical spatial resolution in electron probe microanalysis—Fe-sulfides
- Zircon geochronological and geochemical insights into pluton building and volcanic-hypabyssal-plutonic connections: Oki-Dōzen, Sea of Japan—A complex intraplate alkaline volcano
- Using cathodoluminescence to identify oscillatory zoning of perthitic K‑feldspar from the equigranular Toki granite
- Influence of intensive parameters and assemblies on friction evolution during piston-cylinder experiments
- Formation process of Al-rich calcium amphibole in quartz-bearing eclogites from The Sulu Belt, China
- Helvine-danalite mineralogy of the Dulong Sn-Zn polymetallic deposit in southeast Yunnan, China
- Native gold enrichment process during growth of chalcopyrite-lined conduits within a modern hydrothermal chimney (Manus Basin, PNG)
- Pliniusite, Ca5(VO4)3F, a new apatite-group mineral and the novel natural ternary solid-solution system pliniusite–svabite–fluorapatite
- Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada
- A revised analysis of ferrihydrite at liquid helium temperature using Mössbauer spectroscopy
- First find of merrillite, Ca3(PO4)2, in a terrestrial environment as an inclusion in lower-mantle diamond
- New Mineral Names: Hydrous Minerals
- Book Review
- Past to Present. (2020) Edited by Beth N. Orcutt, Isabelle Daniel, and Rajdeep Dasgupta.
Artikel in diesem Heft
- Estimating kaolinite crystallinity using near-infrared spectroscopy: Implications for its geology on Earth and Mars
- The interplay between twinning and cation inversion in MgAl2O4-spinel: Implications for a nebular thermochronometer
- The effect of fluorine on reaction-rim growth dynamics in the ternary CaO-MgO-SiO2 system
- Seeing through metamorphic overprints in Archean granulites: Combined high-resolution thermometry and phase equilibrium modeling of the Lewisian Complex, Scotland
- Interphase misorientation as a tool to study metamorphic reactions and crystallization in geological materials
- Trace element partitioning between olivine and melt in lunar basalts
- Solving the iron quantification problem in low-kV EPMA: An essential step toward improved analytical spatial resolution in electron probe microanalysis—Fe-sulfides
- Zircon geochronological and geochemical insights into pluton building and volcanic-hypabyssal-plutonic connections: Oki-Dōzen, Sea of Japan—A complex intraplate alkaline volcano
- Using cathodoluminescence to identify oscillatory zoning of perthitic K‑feldspar from the equigranular Toki granite
- Influence of intensive parameters and assemblies on friction evolution during piston-cylinder experiments
- Formation process of Al-rich calcium amphibole in quartz-bearing eclogites from The Sulu Belt, China
- Helvine-danalite mineralogy of the Dulong Sn-Zn polymetallic deposit in southeast Yunnan, China
- Native gold enrichment process during growth of chalcopyrite-lined conduits within a modern hydrothermal chimney (Manus Basin, PNG)
- Pliniusite, Ca5(VO4)3F, a new apatite-group mineral and the novel natural ternary solid-solution system pliniusite–svabite–fluorapatite
- Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada
- A revised analysis of ferrihydrite at liquid helium temperature using Mössbauer spectroscopy
- First find of merrillite, Ca3(PO4)2, in a terrestrial environment as an inclusion in lower-mantle diamond
- New Mineral Names: Hydrous Minerals
- Book Review
- Past to Present. (2020) Edited by Beth N. Orcutt, Isabelle Daniel, and Rajdeep Dasgupta.