Dear colleagues,
We invite you to submit an abstract to Session 9.2 - 'Tracking
subduction-zone fluids via minerals: Advances in natural and experimental
approaches' for the IMA (International Mineralogical Association) general
meeting in Nanjing, China (August 20–24, 2026). The session description can
be found below.
We are pleased to announce that lectures will be provided by the following
keynote and invited speakers.
- Keynote speaker: Yi-Xiang Chen (University of Science and Technology of
China)
- Invited speakers: Ryosuke Oyanagi (Kokushikan University) and *Marija
Putak Juriček *(University of Arizona)
The abstract deadline is *March 15th, 2026. *Visit the website (
https://ima2026.nju.edu.cn/_s806/main.psp) for more details. If you have
any questions, do not hesitate to contact us.
We look forward to your contributions and hope to see you in Nanjing!
Best regards,
Ryo Fukushima (Kochi Institute for Core Sample Research, JAMSTEC / Visiting
scholar at Goethe University Frankfurt)
Yongsheng Huang (Guangzhou Institute of Geochemistry, Chinese Academy of
Sciences)
Jesse B. Walters (University of Graz)
Tatsuki Tsujimori (Tohoku University)
----- Session description -----
Supercritical fluids play critical roles in global mass cycling and
geodynamic processes within subduction zones. Field observations from
high-pressure and ultrahigh-pressure orogenic belts along convergent
margins reveal pervasive fluid flow, extensive fluid-rock interactions, and
clear relationships between rock deformation and fluid migration. Isotopic
analyses of minerals in slab-derived metamorphic rocks and associated
mantle materials provide key constraints on deep-sourced fluid origins.
Recent advances in thermodynamic datasets for high-pressure fluids now
enable more refined characterization of aqueous fluid compositions, while
high-pressure and high-temperature experimental simulations offer valuable
insights into fluid distribution and inventory in Earth's interior.
Improved understanding of fluid distribution, migration mechanisms, and
their geochemical-geophysical responses enhances our knowledge of global
material cycles and geodynamics.
This session highlights recent advances in understanding fluid
properties and behavior in subduction zones, particularly encouraging
contributions that investigate fluid chemistry, fluid-rock reaction
kinetics, and fluid migration mechanisms across scales (meter to nanometer)
through petrological, geochemical, experimental, tectonic, and numerical
modeling approaches, aiming to foster interdisciplinary collaboration in
subduction zone research.
--
Ryo Fukushima, Ph.D.
Postdoctoral Researcher/JSPS Research Fellow
Kochi Institute for Core Sample Research, JAMSTEC
ryofuku@jamstec.go.jp
https://orcid.org/0000-0003-2683-6757
Dear colleagues,
We invite you to submit an abstract to *Session 9.2 - 'Tracking
subduction-zone fluids via minerals: Advances in natural and experimental
approaches'* for the IMA (International Mineralogical Association) general
meeting in Nanjing, China (August 20–24, 2026). The session description can
be found below.
We are pleased to announce that lectures will be provided by the following
keynote and invited speakers.
- Keynote speaker: *Yi-Xiang Chen* (University of Science and Technology of
China)
- Invited speakers: *Ryosuke Oyanagi* (Kokushikan University) and *Marija
Putak Juriček *(University of Arizona)
The abstract deadline is *March 15th, 2026. *Visit the website (
https://ima2026.nju.edu.cn/_s806/main.psp) for more details. If you have
any questions, do not hesitate to contact us.
We look forward to your contributions and hope to see you in Nanjing!
Best regards,
Ryo Fukushima (Kochi Institute for Core Sample Research, JAMSTEC / Visiting
scholar at Goethe University Frankfurt)
Yongsheng Huang (Guangzhou Institute of Geochemistry, Chinese Academy of
Sciences)
Jesse B. Walters (University of Graz)
Tatsuki Tsujimori (Tohoku University)
----- Session description -----
Supercritical fluids play critical roles in global mass cycling and
geodynamic processes within subduction zones. Field observations from
high-pressure and ultrahigh-pressure orogenic belts along convergent
margins reveal pervasive fluid flow, extensive fluid-rock interactions, and
clear relationships between rock deformation and fluid migration. Isotopic
analyses of minerals in slab-derived metamorphic rocks and associated
mantle materials provide key constraints on deep-sourced fluid origins.
Recent advances in thermodynamic datasets for high-pressure fluids now
enable more refined characterization of aqueous fluid compositions, while
high-pressure and high-temperature experimental simulations offer valuable
insights into fluid distribution and inventory in Earth's interior.
Improved understanding of fluid distribution, migration mechanisms, and
their geochemical-geophysical responses enhances our knowledge of global
material cycles and geodynamics.
This session highlights recent advances in understanding fluid
properties and behavior in subduction zones, particularly encouraging
contributions that investigate fluid chemistry, fluid-rock reaction
kinetics, and fluid migration mechanisms across scales (meter to nanometer)
through petrological, geochemical, experimental, tectonic, and numerical
modeling approaches, aiming to foster interdisciplinary collaboration in
subduction zone research.
--------------------
--
Ryo Fukushima, Ph.D.
Postdoctoral Researcher/JSPS Research Fellow
Kochi Institute for Core Sample Research, JAMSTEC
ryofuku@jamstec.go.jp
https://orcid.org/0000-0003-2683-6757