{"id":22526,"date":"2021-02-17T14:49:02","date_gmt":"2021-02-17T13:49:02","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=22526"},"modified":"2026-01-14T16:00:33","modified_gmt":"2026-01-14T15:00:33","slug":"volcanic-and-magmatic-processes","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/research\/teams\/volcanic-and-magmatic-processes\/","title":{"rendered":"Volcanic and Magmatic Processes"},"content":{"rendered":"

[et_pb_section fb_built=”1″ _builder_version=”4.16″ _module_preset=”default” custom_padding=”40px|||||” global_colors_info=”{}”][et_pb_row column_structure=”3_5,2_5″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”3_5″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ _module_preset=”default” custom_margin=”-2px|||||” global_colors_info=”{}”]<\/p>\n

Team Leader: Graham Hill<\/h4>\n

 <\/p>\n

Research Focus<\/strong><\/p>\n

The Volcanic and Magmatic Processes (VMP) group’s research focus is to better understand the eruptive dynamics of volcanic systems, the generation of magmas, and the relationship between magmatic systems and lithospheric tectonics\/crustal evolution. The study of fundamental volcano\u2010magmatic processes is complex and occurs over multiple scales and depths necessitating a broad group of research methods (geophysical analysis, numerical & analogue modelling, field and laboratory observations) to provide an integrated picture of the processes controlling magma generation through eruption.<\/p>\n

The main research areas are (1) magma propagation and reservoir dynamics, (2) tectonic controls on magmatic process, and (3) eruption dynamics. A second focus of the group is the role of geofluids in geologic processes including mineralization and evolution of Archean craton, salt tectonics, and extensional systems.<\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”2_5″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

Ongoing Projects:<\/h4>\n

Digitial twin of a magmatic system (PI – Annen: GACR)<\/p>\n

Post collisional volcanism – a record of lithospheric mantle evolution (PI – Hill: GACR, DFG, SNSF)<\/p>\n

UNDERCOVER: Unified Novel Deep ExploRation for Critical Ore discoVERy
(PI – Hill: Horizons Europe)<\/p>\n

Structure and dynamics of shallow salt sheet extrusion investigated by
magnetotellurics, gravity and analog modelling (PI – Hill: GACR)<\/p>\n

Formation, extent and duration of permeable crystal suspensions in the
cortical column (PI – Annen: GACR)<\/p>\n

Mount Erebus a window into Alkalic volcanic systems (Hill \u2013 PI: Royal Society of New Zealand)<\/p>\n

Side-stepping the viscosity density trap: the interaction of andesitic and rhyolite volcanism the Novarupta \u2013 Mount Katmai system, Alaska (Hill \u2013 PI: Lumina Quaeruntur)<\/p>\n

D-Rex: Deposit to regional exploration of Archean cratonic magmatic mineralization (Hill \u2013 PI: ERAMIN2 ERC)<\/p>\n

GOLETA: The role of anisotropy in the Antarctic Mantle on isostatic adjustment and sea level rise (Hill \u2013 CoI: Spanish Ministry of Science)<\/p>\n

Comparison of geophysical and geological structures of the Western Carpathian lithosphere with other orogenic areas in Europe (Klanica \u2013 PI: Czech Academy of Sciences)<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n

People<\/strong><\/p>\n\n\n\n\n\n\n\n\n\n\n\n
\"\"<\/td>\nGraham J. Hill<\/a><\/td>\nPhD<\/td>\nSenior researcher (team leader)<\/td>\nElectromagnetics, magmatic processes & volcanism, active tectonics & rift evolution, Archean geodynamics & mineralization<\/td>\n<\/tr>\n
\"\"<\/td>\nCatherine Annen<\/a><\/td>\nPhD<\/td>\nResearcher<\/td>\nCatherine Annen is using numerical simulation to investigate how magma chambers form, how magmas differentiate, and how magmatic systems work at the scale of the crust<\/td>\n<\/tr>\n
\"\"<\/td>\nSv\u011btlana Kov\u00e1\u010dikov\u00e1<\/a><\/td>\nIng, PhD<\/td>\nResearcher<\/td>\nElectromagnetics, electrical conductivity modelling<\/td>\n<\/tr>\n
\"\"<\/td>\nRadek Klanica<\/a><\/td>\nMgr, PhD<\/td>\nResearcher<\/td>\nElectromagnetics, magnetics, tectonics, maar structures<\/td>\n<\/tr>\n
\"\"<\/td>\nHana Hanzl\u00edkov\u00e1<\/a><\/td>\nRNDr, PhD<\/td>\nResearcher<\/td>\nSpace weather, archival geomagnetic measurements<\/td>\n<\/tr>\n
\"\"<\/td>\nJuraj Kyselica<\/a><\/td>\nMgr, PhD<\/td>\nResearcher<\/td>\nGeological fluid mechanics, phase-change processes, partially-solidified systems, flows in porous media, magnetohydrodynamics<\/td>\n<\/tr>\n
\"\"<\/td>\nElia Altimani<\/td>\nPhD student<\/td>\nResearcher<\/td>\nVolcanic and Magmatic Processes<\/td>\n<\/tr>\n
\"\"<\/td>\nC\u00e9sar Daniel Castro<\/a><\/td>\nPhD student<\/td>\nResearcher<\/td>\nElectromagnetic exploration, geophysical modeling, volcanic and magmatic processes, electrical anisotropy, time series processing, EM transfer function analysis<\/td>\n<\/tr>\n
\"\"

Oplus_131074<\/p><\/div><\/td>\n

Alice Wantz<\/td>\nPhD student<\/td>\nResearcher<\/td>\nModelling the feedback effect between dyke injections and sill growth<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

\u00a0<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,1_4,1_4,1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/02\/web-obr1.jpg” title_text=”Web Obr1″ show_in_lightbox=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/02\/web-obr2.jpg” title_text=”Web Obr2″ show_in_lightbox=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/02\/web-obr3.jpg” title_text=”Web Obr3″ show_in_lightbox=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/02\/web-obr5.jpg” title_text=”Web Obr5″ show_in_lightbox=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,1_4,1_4,1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

Aerial view of Mount Erebus, Ross Island, Antarctica (photo: GJ Hill)
<\/em><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

Mount Katmai site of the largest eruption of the 20th<\/sup> century where contemporaneous eruption occurred at both Mount Katmai (pictured) and 10 km away a the new Novarupta vent, Alaska, USA (photo: GJ Hill)
<\/em><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

MT measurements to image the West Antarctic Rift System, Antarctica (photo: GJ Hill)
<\/em><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

MT measurements at the Lusatian Fault near Je\u0161t\u011bd, Czech Republic (photo – R. Klanica, 2019)<\/em><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,1_4,1_4,1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/02\/obr4.jpg” title_text=”Obr4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,1_4,1_4,1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

MT measurements at Mount St Helens, USA (photo: GJ Hill)<\/em><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"

Team Leader: Graham Hill   Research Focus The Volcanic and Magmatic Processes (VMP) group’s research focus is to better understand the eruptive dynamics of volcanic systems, the generation of magmas, and the relationship between magmatic systems and lithospheric tectonics\/crustal evolution. The study of fundamental volcano\u2010magmatic processes is complex and occurs over multiple scales and depths […]<\/p>\n","protected":false},"author":2,"featured_media":14269,"parent":27543,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[],"class_list":["post-22526","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"\nVolcanic and Magmatic Processes - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/volcanic-and-magmatic-processes\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Volcanic and Magmatic Processes - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"Team Leader: Graham Hill   Research Focus The Volcanic and Magmatic Processes (VMP) group's research focus is to better understand the eruptive dynamics of volcanic systems, the generation of magmas, and the relationship between magmatic systems and lithospheric tectonics\/crustal evolution. 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