固体地球科学(S) | |||
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セッション小記号 | 固体地球化学(GC) | ||
セッションID | S-GC37 | ||
タイトル | 和文 | Volatiles in the Earth - from Surface to Deep Mantle | |
英文 | Volatiles in the Earth - from Surface to Deep Mantle | ||
タイトル短縮名 | 和文 | Volatiles in the Earth | |
英文 | Volatiles in the Earth | ||
代表コンビーナ | 氏名 | 和文 | 角野 浩史 |
英文 | Hirochika Sumino | ||
所属 | 和文 | 東京大学先端科学技術研究センター | |
英文 | Research Center for Advanced Science and Technology, The University of Tokyo | ||
共同コンビーナ 1 | 氏名 | 和文 | Antonio Caracausi |
英文 | Antonio Caracausi | ||
所属 | 和文 | National Institute of Geophysics and Volcanology | |
英文 | National Institute of Geophysics and Volcanology | ||
共同コンビーナ 2 | 氏名 | 和文 | 清水 健二 |
英文 | Kenji Shimizu | ||
所属 | 和文 | 海洋研究開発機構 高知コア研究所 | |
英文 | Kochi Institute of Core Research, Japan Agency for Marine-Earth Science and Technology | ||
共同コンビーナ 3 | 氏名 | 和文 | 羽生 毅 |
英文 | Takeshi Hanyu | ||
所属 | 和文 | 海洋研究開発機構 海域地震火山部門 | |
英文 | Japan Agency for Marine-Earth Science and Technology, Research Institute for Marine Geodynamics | ||
発表言語 | E | ||
スコープ | 和文 |
Volatiles play an essential role in the dynamic and chemical processes in the Earth's interior. The presence of volatiles drastically changes the mineral stability and rheological behavior of the rocks. Chemical fractionation, such as partial melting, hydration, and dehydration, is controlled by volatiles in the rocks. Volatiles enhance the production of magma and drive their ascent and volcanic eruption. The atmosphere and hydrosphere have been generated by various degassing events from the mantle through volcanism. Some volatiles in the Earth's surface have been suggested to be recycled back into the mantle beyond subduction zones. Although the significance of volatiles in the Earth's evolution has been recognized, each of these processes is poorly constrained. We therefore welcome contributions from experimental, observational, and modeling studies that help shed light on the behavior, chemical/physical characteristics, and flux/budget of volatiles, such as hydrogen, carbon, nitrogen, noble gases, halogens, and sulfur. We encourage studies linking the behavior of multiple volatile elements and their isotopic compositions. Studies investigating the linkage between volatile and solid geochemical tracers, the phase equilibria of volatile-bearing mantle assemblages, and the effect of volatiles on the physical properties of the mantle are also welcome. |
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英文 |
Volatiles play an essential role in the dynamic and chemical processes in the Earth's interior. The presence of volatiles drastically changes the mineral stability and rheological behavior of the rocks. Chemical fractionation, such as partial melting, hydration, and dehydration, is controlled by volatiles in the rocks. Volatiles enhance the production of magma and drive their ascent and volcanic eruption. The atmosphere and hydrosphere have been generated by various degassing events from the mantle through volcanism. Some volatiles in the Earth's surface have been suggested to be recycled back into the mantle beyond subduction zones. Although the significance of volatiles in the Earth's evolution has been recognized, each of these processes is poorly constrained. We therefore welcome contributions from experimental, observational, and modeling studies that help shed light on the behavior, chemical/physical characteristics, and flux/budget of volatiles, such as hydrogen, carbon, nitrogen, noble gases, halogens, and sulfur. We encourage studies linking the behavior of multiple volatile elements and their isotopic compositions. Studies investigating the linkage between volatile and solid geochemical tracers, the phase equilibria of volatile-bearing mantle assemblages, and the effect of volatiles on the physical properties of the mantle are also welcome. |
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発表方法 | 口頭および(または)ポスターセッション | ||
ジョイントセッション | EGU | ||
招待講演 |
Ching-Chou FU (Institute of Earth Sciences, Academia Sinica) Soyeon Kim (Seoul National University) 小長谷 智哉 (東京科学大学) Antonio Paonita (istituto nazionale di geofisica e vulcanologia) |
時間 | 講演番号 | タイトル | 発表者 |
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口頭発表 5月27日 AM1 | |||
9:00 - 9:15 | SGC37-01 | Isotopic Modification of ∂13C via CO2-Mineral Equilibria: Implications on the origin of CO2 degassing at Earth’s surface. | Antonio Caracausi |
9:15 - 9:30 | SGC37-02 | From Slab to Mantle: Phengite’s Role in Deep Earth Fluorine and Chlorine Delivery | Yu Wang |
9:30 - 9:45 | SGC37-03 | Large-scale loss of the Earth's primordial atmosphere implied by carbon metal/silicate partitioning | 土屋 卓久 |
9:45 - 10:00 | SGC37-04 | The distribution and cycling of water and carbon in the global asthenospheric mantle revealed by machine learning | Liu liujia85@zju.edu.cn |
10:00 - 10:15 | SGC37-05 | Boron, lithium and chlorine systematics of geothermal fluids of Mexico: mantle and crustal sources | Daniele Luigi Pinti |
10:15 - 10:30 | SGC37-06 | Recycling mercury in a convergent margin of subducting Philippine Sea Plate at Southwest Japan | 益田 晴恵 |
口頭発表 5月27日 PM1 | |||
13:45 - 14:15 | SGC37-07 | Persistent crustal CO2 emissions following the 2022 M6.8 Chihshang earthquake sequence in eastern Taiwan | Ching-Chou FU |
14:15 - 14:30 | SGC37-08 | The diverging subduction of tearing slab controls the deep carbon recycling efficiency: Geochemical evidence from the SE Tibetan Plateau | Yingchun Wang |
14:30 - 14:45 | SGC37-09 | イタリアのオフィオライト中のオフィカーボネイトに含まれる流体包有物の水素酸素同位体比が記録する中央海嶺下の熱水 | 川本 竜彦 |
14:45 - 15:00 | SGC37-10 | Impact of volcanic volatile fluxes on Mesozoic terrestrial biotas in northern China | Lu Wang |
15:00 - 15:15 | SGC37-11 | かんらん石メルト包有物を用いたマグマ生成過程の解明: 中国地方,阿武単成火山群を例として | 吉村 雪香 |
口頭発表 5月27日 PM2 | |||
15:30 - 16:00 | SGC37-12 | Magma Degassing and Explosive Eruption of Hunga Volcano | Soyeon Kim |
16:00 - 16:15 | SGC37-13 | 2021年福徳岡ノ場の爆発的噴火に関与したH2OとCaに富む玄武岩質メルト | 萩原 雄貴 |
16:15 - 16:30 | SGC37-14 | Helium, argon and nitrogen systematics in the KR1 segment of the Australian-Antarctic Ridge: Constraints on enriched sources for the Zealandia–Antarctic mantle domain | Donghwan Kim |
16:30 - 16:45 | SGC37-15 | MORB-like mantle noble gases beneath the oldest oceanic plate | 小長谷 智哉 |
16:45 - 17:00 | SGC37-16 | Halogen and noble gas systematics of mantle xenoliths from the rear-arc regions in Eastern Asia | 角野 浩史 |
講演番号 | タイトル | 発表者 |
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ポスター発表 5月27日 PM3 | ||
SGC37-P01 | Temporal variations of helium isotopes observed in earthquake swarm regions on the Noto Peninsula, central Japan | 長谷川 未侑 |
SGC37-P02 | Noble gas geochemistry of melt inclusions in pumice of the latest magmatic eruption since 2022 of Ioto island (Iwo-Jima) | 山本 蒼邦 |
SGC37-P03 | Noble Gas Isotopic Signatures of the Pacific Lithosphere: Insights from Petit-Spot Mantle Xenoliths | 新井 孝彰 |
SGC37-P04 | Water contents and pressures estimated from melt inclusions in zircon of the Cretaceous Habu granitoid pluton, San-yo Belt, southwest Japan. | 熊谷 汐莉 |
SGC37-P05 | Geochemistry and geodynamic implications of High-Mg diorites from the Lohit Plutonic Complex of eastern Arunachal Trans-Himalaya, north eastern India | LEIPHRAKPAM LEMBA SINGH |
SGC37-P06 | 高圧変成岩中の流体包有物により直接的に制約した,沈み込むスラブ由来の深部流体安定同位体組成 | 吉田 健太 |
SGC37-P07 | Oxybarometry and hygrothermobarometry for granites using zircon and melt inclusions: examples of the Kaikomagatake, Miuchi, Daito, and Gamano granitoids in Japan | 齊藤 哲 |
SGC37-P08 | 能登半島における基盤岩のヘリウム同位体組成:2024年能登半島地震の前後における地下水化学成分の時間変化の考察 | 長谷川 実咲 |
SGC37-P09 | Contribution of crustal material inferred from δ26Mg ratios from intraplate volcanics of southwest Japan | Bidisha Dey |
SGC37-P10 | Spectroscopic analysis of microdiamonds from Kokchetav, Kazakhstan: Towards the elucidation of the origin of deep mantle fluids through the noble gas isotope analysis | 川村 英彰 |
SGC37-P11 | The volatiles and hydrogen isotopes of high 3He/4He submarine volcanic glass and melt inclusions from Hawaii characterized the water in the deep and primordial Earth | 清水 健二 |
SGC37-P12 | Fumarole geochemistry during the 2021-22 unrest of Vulcano Island (Italy): the magmatic source in the precursory and ongoing phases | Antonio Paonita |
SGC37-P13 | Origin of gases emitted during coal waste self-heating in Upper Silesia, Poland and Czechia – laboratory simulation data | Dariusz Wieclaw |
SGC37-P14 | Depth water variation in the mantle beneath Nushan, SE-edge of Sino-Korean craton | 佐藤 侑人 |
SGC37-P15 | A geochemical study on mantle xenoliths from the eastern Mediterranean: constraints from noble gas isotope systematics | Antonio Caracausi |
SGC37-P16 | Evolving Volcanic Unrest in the Tatun Volcano Group: Linking Microseismic Activity and Geochemical Signals in Northern Taiwan | AITI CHEN |
SGC37-P17 | Chemical and geological CO2 sequestration | Monika Motak |
SGC37-P18 | Functionalized Natural Materials as Catalysts for the Dry Reforming of Methane | Bogdan Samojeden |