Startseite 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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Zircon geochronological and geochemical insights into pluton building and volcanic-hypabyssal-plutonic connections: Oki-Dōzen, Sea of Japan—A complex intraplate alkaline volcano

  • Jane H. Scarrow , Katy J. Chamberlain , Pilar Montero , Matthew S.A. Horstwood , Jun-Ichi Kimura , Yoshihiko Tamura , Qing Chang und Jenni Barclay
Veröffentlicht/Copyright: 27. Juli 2022
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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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Received: 2020-10-18
Accepted: 2021-07-29
Published Online: 2022-07-27
Published in Print: 2022-08-26

© 2022 Mineralogical Society of America

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