IGC Busan Abstract deadline approaching: Session T8-1 convened by Zellmer & Brahm

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From: Georg Zellmer <G.F.Zellmer@xxxxxxxxxxxx>


Dear All,



Please note that abstract submissions will be closed at midnight on 15
March, 2024 (24:00 p.m. KST, UTC/GMT+09).

See here for details about this meeting: https://www.igc2024korea.org/
<https://urldefense.com/v3/__https://www.igc2024korea.org/__;!!IKRxdwAv5BmarQ!c5P66IAM2uesFqt54UW4TXZgBPYEkVid9tkoUsl2YY42_NgNfxeJhDjWbQW9T1LVZUADcE1I7m1D5xnZwfxn_V4GJg$>



Please consider submitting your abstract to session T8-1 convened by
Zellmer and Brahm:



*â??Architecture and Thermal Structure of Translithospheric Magmatic Systemsâ??*



Transcrustal magmatic systems host plutonic rocks, crystal mushes, and
magma reservoirs, connected through a network of dykes and sills. These
systems can also extend into the lithospheric mantle. System architecture
and thermal structure are critical parameters for understanding the genetic
history of intrusive magmatism and the style of volcanic eruptions, as well
as textural and compositional variations in eruptive products.
Understanding the architecture and construction of translithospheric
magmatic systems is therefore a prerequisite for understanding and
mitigating volcanic hazards through the development of appropriate and
effective volcano monitoring strategies. Further, the thermal structure of
these translithospheric magmatic systems governs crystallization behaviour
and concomitant evolution of melt, fluid and gas exsolution from ascending
magmas, brittle versus ductile crustal responses to this ascent, and the
depth and extent of formation of economic mineral deposits.


We invite contributions from a wide range of disciplines that may shed
light on these topics across all tectonic settings, including but not
limited to:

(i) experimental petrology, providing the PTtX-context for observations of
natural samples;

(ii) analytical petrology and geochemistry, including thermobarometric and
geospeedometric studies of intrusive and eruptive products, encompassing
the volatile phases (e.g., hygrometry, melt and fluid inclusion analysis);

(iii) physical volcanology to elucidate links between subvolcanic processes
and eruptive activity;

(iv) thermodynamic and numerical modelling

(v) economic geology;

(vi) geophysics to inform the interpretation of data provided by other
disciplines.


We particularly encourage studies that combine diverse approaches and
demonstrate that collaborative efforts can provide new insights that escape
detection by individual disciplines.



See you in Busan!

Georg Zellmer

Raimundo Brahm


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