10-10-10-10-10-10-10-10-10-10-10 From: "FOULGER, GILLIAN R." <g.r.foulger@xxxxxxxxxxxx> Dear colleague, I bring to your attention EGU 27 April - 2 May 2025, Session TS2.3 New directions on crustal affinities offshore <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fmeetingorganizer.copernicus.org*2FEGU25*2Fsession*2F51747&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700296719*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=h6V*2F0V8RrRsAjHMq7KGVoETpR2hvh3wbKZ*2BrBGtVwyY*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUlJQ!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIeRHTr1FQ$>. Please see the details below. Oceanic islands may also be considered â??offshoreâ?? in this context. Both virtual and in-person attendance is possible. The deadline for abstract submission is 15th January 2025 13.00 CET. More information on how to submit your abstract here: https://www.egu25.eu/programme/how_to_submit.html <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fwww.egu25.eu*2Fprogramme*2Fhow_to_submit.html&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700296719*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=BxSCGliNa*2BeRGj*2FJD0esXL6LlOXahtyYnJ*2BUrY*2FQ7*2Fs*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIehVSwTkA$> Travel support information is here: https://www.egu25.eu/guidelines/supports_and_waivers.html <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fwww.egu25.eu*2Fguidelines*2Fsupports_and_waivers.html&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700296719*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=DCkB*2FHaxSiB4tJ96By13R73xZkNBkbVu5slDqbJt*2FAg*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIeat4WELw$> Kind regards, Gillian R. Foulger *TS2.3: New directions on crustal affinities offshore* Co-organized by GD5 Convener: Jean-Baptiste P. Koehl <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fmeetingorganizer.copernicus.org*2FEGU25*2Fsession*2F51747*23&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700296719*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=xM*2Bbh2iuOeitrEkrq23ag6HqrLdkoWU1Da7RlEaQTVk*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUlJQ!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIch4FRvdg$>*ECS <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fmeetingorganizer.copernicus.org*2FEGU25*2Fsession*2F51747*23&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700452958*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=DVhdin4MY2TDkxKGSzgbuarOfnEQvMW7lnfVUjjNik4*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIdvOiEWkA$>* | Co-conveners: Gillian R. Foulger <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fmeetingorganizer.copernicus.org*2FEGU25*2Fsession*2F51747*23&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700452958*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=DVhdin4MY2TDkxKGSzgbuarOfnEQvMW7lnfVUjjNik4*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIdvOiEWkA$> , Alexander L. Peace <https://urldefense.com/v3/__https://eur01.safelinks.protection.outlook.com/?url=https*3A*2F*2Fmeetingorganizer.copernicus.org*2FEGU25*2Fsession*2F51747*23&data=05*7C02*7Cmantleplumes*40durham.ac.uk*7C5702e3d3ead74e9a0ddf08dd0c259356*7C7250d88b4b684529be44d59a2d8a6f94*7C0*7C0*7C638680077700452958*7CUnknown*7CTWFpbGZsb3d8eyJFbXB0eU1hcGkiOnRydWUsIlYiOiIwLjAuMDAwMCIsIlAiOiJXaW4zMiIsIkFOIjoiTWFpbCIsIldUIjoyfQ*3D*3D*7C0*7C*7C*7C&sdata=DVhdin4MY2TDkxKGSzgbuarOfnEQvMW7lnfVUjjNik4*3D&reserved=0__;JSUlJSUlJSUlJSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!emrV3vYhss7d9fF_y84ugN8hIAbBme9UDIhbVHqFFq27s24a2xQebX9agfWS7Fo6-FlD7ia7dLNbQBCjCIdvOiEWkA$> Ever since the inception of Wegenerâ??s Continental Drift and ensuing plate tectonics, the Earthâ??s crust has been described using a bimodal classification: oceanic versus continental. However, after decades of advances in subsurface imaging, it is clear this is an over-simplification. The crust offshore may be hyperextended and/or extensively intruded continental crust, and continental microplates may be common. Recent advances in geophysical imaging, dredging and drilling-based exploration have evidenced features like dykes, sills, and Seaward-Dipping Reflectors and tectonic structures such as folds, brittle faults, and shear zones, revealing details of large crustal transects offshore. We welcome contributions from all fields of geoscience that relate to the extent of continental, oceanic, and hybrid crust beneath continental shelves and in the oceans. Contributions may be based on observations, numerical modelling or theory, and may derive from any part of the world. We also welcome contributions focusing on the long-term processes from orogenesis to rifting and transform faulting, and bring new perspectives to disputed areas. 10-10-10-10-10-10-10-10-10-10-10 ------------------------------
