1-1-1-1-1-1-1-1-1-1-1-1-1-1 From: Sam Poppe <sam35poppe@xxxxxxxxx> Dear colleagues, Are you working on magma emplacement in sedimentary basins and interactions between igneous systems and sedimentary rocks? Please consider submitting your abstract to our session on "Magma-rock interactions in sedimentary basins" to be held at the 18th Workshop of the International Lithosphere Program - Task Force Sedimentary Basins to be held in Kraków, Poland from 7-11 October 2024 ( https://urldefense.com/v3/__https://ilp-krakow2024.pl/__;!!IKRxdwAv5BmarQ!dNFoi4r16afh7NGG28kUOafMTHimKqHOvRC8gOP3Ot3PVVlvO-tPSnzWWo_dhdZHF4WoBpiE27ShdtRM4vc3QhSXmA$ ). Our keynote speaker will be Christophe Galerne (University of Bremen). The meeting will host a range of topics related to sedimentary basins from stress, strain and fluids in sedimentary basins to energy resources and geohazards, and pre- and post-workshop field trips in Poland´s spectacular salt mines and sequences from Neoproterozoic rifting to Late Cretaceous basin inversion. Please submit your abstracts (free-of-charge) before 30 July. Early registration ends shortly on 30 June. Looking forward to seeing many of you in Kraków in October to discuss magma versus sediments! Sam Poppe and PaweÅ? Poprawa, for the conveners *Session summary* "Magma-rock interactions in sedimentary basins" Program group "Stress, strain and fluids in sedimentary basins" Regional magma intrusion cycles can significantly alter the architecture and fluid circulation in sedimentary basins, while magma-induced stresses and strains interact with regional tectonic stresses to which a basin is subjected. Multidisciplinary study across branches of geoscience is often required to understand the full scope of the impact igneous systems have on sedimentary basins. This session invites contributions investigating igneous and volcanic systems in sedimentary basins, such as magma emplacement modes in heterogenous rock sequences, magma-induced deformation, thermal and chemical magma-sediment interactions, hydrothermal fluid circulation, the impact on the thermal history of basins, magma-sediment mineral trapping, and implications for geothermal resources, CO2 storage, the climate, and volcanic unrest. Approaches and multidisciplinary combinations from field observations, mineralogical and geochemical analyses, geophysical investigations to experimental and numerical modelling are particularly welcome. 1-1-1-1-1-1-1-1-1-1-1-1-1-1 ------------------------------
