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Geodynamics

Geodynamics

Mantle, Mountains and Molluscs

Mantle, Mountains and Molluscs

Geodynamic models and landscape evolution models are becoming important tools to quantify the formation and development of paleogeographic features, contributing to our understanding of the patterns of biodiversity evolution. Earth, a dynamic system The Earth’s surface works as a dynamic system and is continuously sculpted through the geological timescale by weathering, wind, rivers, and many …[Read More]

T for temperature in seismic [T]omography and more

T for temperature in seismic [T]omography and more

Seismic tomography, a powerful geophysical technique, is like the Sherlock Holmes of the Earth’s interior. It helps us uncover crucial information about the lithosphere and mantle, including temperature and density distributions. Understanding these physical properties is vital for a wide range of geological applications, from identifying regions of strain localization to assessing geothermal potential. In …[Read More]

Dual inward dipping subduction: A Christmas Cracker Model

Dual inward dipping subduction: A Christmas Cracker Model

A recent research finds that dual inward dipping subduction framework, after considering thermal dependent deformation mechanisms, can pull apart the middle overriding plate (Lei and Davies, 2023), just like pulling Christmas crackers from both ends! Dual inward dipping subduction (DIDS) occurs when the overriding plate is decoupled with two subducting slabs dipping towards each other. …[Read More]

Exploring Kolumbo: Unveiling the Secrets of a Submarine Volcano

Exploring Kolumbo: Unveiling the Secrets of a Submarine Volcano

Santorini Island without a doubt is one of the top worldwide destinations, taking our breath away with its unparalleled beauty. However, from the geological perspective as well, this mystifying island can reveal hidden secrets of the past and pave the way for our future. In this week’s blog, Associate Professor Paraskevi Nomikou, the 2023 awardee …[Read More]

Modelling CPO evolution with D-Rex

Modelling CPO evolution with D-Rex

As a result of Earth’s mantle convection, rocks in the earth’s interior flow and develop a crystallographic texture. These textures reveal the planet’s thermal and tectonic history and are responsible for the viscous anisotropy, which can be used to study the planet’s deeper recesses that are not visible through other means. This necessitates the use …[Read More]