Mar Moragas Rodriguez

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

What can we learn from salt-basins field analogues? The Moroccan Central High Atlas revisited Mar Moragas (Postdoktor ZechTec project, GBS) The Central High Atlas was classically regarded as a failed Mesozoic rift arm subject to Alpine inversion, folding and thrusting …

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Ann Rowan

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Quantifying terrestrial palaeoclimate variability from ice-marginal moraines Glaciated landscapes contain moraines that record past glacier extent from which we can (in some cases) infer palaeoclimate. However, to do so, we need to bear in mind that glacier response to climate …

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Simone Masoch (Dipartimento di Geoscienze, Università degli Studi di Padova, Padua, Italy)

Structural evolution and architecture of an exhumed crustal-scale seismogenic fault (Bolfin Fault Zone, Atacama Fault System, Chile) Simone Masoch The architecture and spatio-temporal evolution of brittle fault zones play a pivotal role in earthquake mechanics, by controlling, for instance, the …

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Grace Shephard

s-Inking the rainbow - introducing two initiatives for generating better science graphics Grace Shephard The adage, “a picture is worth a thousand words,” is wholly applicable to the (geo)sciences. Whether in publications, talks, teaching or press-releases, the use of effective graphics is paramount …

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Ujjwal Shekhar

Ujjwal Shekhar Microseismic wavefield modeling using the integral equation method Induced seismicity is commonly associated with activities like conventional and unconventional oil/gas production, enhanced geothermal systems, carbon sequestration, hydraulic fracturing, etc. Fluid injection/extraction affects the pore pressure within the rockmass and …

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Umut Isikalp

Sedimentology and Stratigraphy of the Cambrian and Ordovician Deposits in SE Turkey Umut Isikalp

AGU 2022 practice

Thomas Theunissen - Oblique continental rifting. Insights from 3-D forward geodynamic modelling coupled with surface processes and application to the Equatorial passive margins formation. Sebastian Wolf - How high do mountains grow? quantifying growth and decay of topography in collision …

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