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on our recent discovery that impact ejecta produces a unique hundred-metre-scale irregular cellular structure when it interacts with mid-latitude debris covered glaciers. Our pilot work established the
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mechanisms: far-field plate tectonics (e.g., Atlantic ridge push, etc.), gravitational potential energy (topography and lithospheric structure), Quaternary glacial isostatic adjustment (Fennoscandian and
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for the destruction of pathogens are structures sought in photomedicine to develop a spatiotemporal approach to treatment. This is at the heart of the project, which aims to prepare a new family of Bodipy dyes
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historical and recent earthquakes, indicating the reactivation of inherited crustal structures. This PhD project aims to quantify geomorphic signatures of tectonic activity using high-resolution topographic
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electronic structure methods for the above-described properties. In more details, this will require the development of an automated approach that allows identifying the excited-states across several levels