Dellefant, Fabian

PostDoc Researcher, ERC DiverseNile Project

Fabian.Dellefant@lmu.de

Fabian Dellefant completed a PhD at the Department of Earth and Environmental Sciences at the Ludwigs-Maximilians-Universität Munich focusing on shock effects of Fe-Ti-oxides generated by meteorite impacts, which can contribute to km-scale magnetic anomalies. In his work, the application of Raman spectroscopy plays a central role, which he now utilizes to investigate maximum firing temperatures of archaeological ceramic samples in the framework of the DiverseNile project. Fabian possesses extensive experience in characterizing materials from various perspectives, including (magneto-)mineralogy, crystallography, and geology. He intends to leverage this expertise in investigating the petrography and potential provenance of Egyptian sandstone building materials.

Main Areas of Research

Characterization of geomaterials, Raman spectroscopy of charcoal, Archaeometry, Impact geology, (Magneto-)Mineralogy, Petrography

Methods

Optical microscopy (transmitted and reflected light); Raman spectroscopy; Scanning electron microscopy (+electron backscattered diffraction)

Education

01/2020 – 01/2024     Ludwig-Maximilians-Universität Munich                           

• PhD in the field of impact geology

10/2016 – 03/2019     Ludwig-Maximilians-Universität Munich & Technical University of Munich          

• Course: MSc Geomaterials and Geochemistry

09/2013 – 03/2016     Ludwig-Maximilians-Universität Munich & Technical University of Munich                                                                                                                              

• Course: BSc Geosciences (focus on Mineralogy)

10/2012 – 09/2013     Ruhr-Universität Bochum                                                               

• Course: BSc Geosciences

Publications

Brückner L. M., Dellefant F., and Trepmann C. A. (2024) Quartz cleavage fracturing and subsequent recrystallization along the damage zone recording fast stress unloading. Journal of Structural Geology 178:105008. https://doi.org/10.1016/j.jsg.2023.105008.

Dellefant, F., Trepmann, C.A., Gilder, S.A., Sleptsova, I. V, Kaliwoda, M., and Weiss, B.P.(2022) Ilmenite  and magnetite microfabrics in shocked gneisses from the Vredefort impact structure, South Africa. Contributions to Mineralogy and Petrology, 5. https://doi.org/10.1007/s00410-022-01950-5

Dellefant, F., Trepmann, C.A., Schmahl, W.W., Gilder, S.A., Sleptsova, I. V., and Kaliwoda, M. (accepted) Ilmenite phase transformations in suevite from the Ries impact structure (Germany) record evolution in pressure, temperature, and oxygen fugacity conditions. American Mineralogist. https://doi.org/10.2138/am-2023-8985

Dellefant F., D’Ercole G., Budka J., and Kaliwoda M. (2023) Differentiation of Late Bronze Age Nubian- and Egyptian-style ceramics from northern Sudan by manufacturing firing   temperatures using Raman Spectroscopy. Journal of Archaeological Science: Reports 52:104233. https://doi.org/10.1016/j.jasrep.2023.104233.

Dellefant, F., Seybold, L., Trepmann, C.A., Gilder, S.A., Sleptsova, I. V., Hölzl, S., and Kaliwoda, M.  (accepted) Emplacement of shocked basement clasts during crater excavation in the Ries impact structure. International Journal of Earth Sciences.

Seybold, L., Trepmann, C.A., Hölzl, S., Pollok, K., Langenhorst, F., Dellefant, F., and Kaliwoda, M. (2023) Twinned calcite as an indicator of high differential stresses and low shock pressure conditions during impact cratering. Meteoritics & Planetary Science, 19.   doi.org/10.1111/maps.14056

Sleptsova I. V., Gilder S. A., Dellefant F., Trepmann C. A., Ahanin N., and Pohl J. (2024).    Thermal and Structural History of Impact Ejecta Deposits, Ries Impact Structure, Germany. Journal of  Geophysical Research: Solid Earth 129:1–23. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023JB027460.

Trepmann, C.A., Dellefant, F., Kaliwoda, M., Hess, K.U., Schmahl, W.W., and Hölzl, S. (2020) Quartz and cristobalite ballen in impact melt rocks from the Ries impact structure, Germany, formed by dehydration of shock-generated amorphous phases. Meteoritics and Planetary Science, 55, 2360–2374. https://doi.org/10.1111/maps.13590

Complete CV