CLR person interests, research and publications
Researcher

About me
After completing an intergrated masters of geology (MGeol.) degree at the University of Leicester in the United Kingodm, I went on to study for a PhD. at Charles University in Prague. My PhD. research involved a metamorphic and geochronological study of the basement rocks of the Kabul Block in Afghanistan.
I started at the Centre for Lithospheric Research in January 2016 where my research focusses on the metamorphism of high-grade rocks in the northwest Bohemian Massif. Although principally a metamorphic petrologist, I combine elements of geochemistry, isotope geochronology and structural geology into my research.
Research Interests
- Metamorphic petrology and thermodynamic phase-equilibria modelling
- Geochronological dating of igneous and metamorphic processes
- The Variscan orogeny in the north west Bohemian massif
My research is focussed on reconstructing Neoproterozoic and Paleozoic orogenic systems responsible for the consolidation of the terranes of Central and Western Europe. These terranes record a near complete record from the break-up of the Early Neproterozoic supercontinent Rodinia to the consolidation of the Late Paleozoic supercontinent Pangea and understanding their evolution provides important advances to our understanding of the supercontinent cycle. These works are primarily carried out in high-grade terranes that experienced complex and often poly-metamorphic evolution and include structural-petrological (e.g. Collett et al. 2018 - Lithos), detrital zircon geochronological (e.g. Collett et al. 2020 - Gondwana Research), and whole-rock chemical and isotopic studies (e.g. Collett et al. 2021 - JGSL) as well as being involved in large-scale correlative studies (e.g. Martínez Catalan, Collett et al. 2020 - IJES).
In addition I have also been involved in several studies utilising the same methods as above in both Central Asia and the Himalaya and have collaborated with researchers in Czech Republic, Poland, Austria, France, Spain, USA, China, and Afghanistan.
Research projects
The Variscan Orogenic Belt developed in response to Devonian-Carboniferous collision between Laurussia and Gondwana and closure of the early Paleozoic Rheic Ocean. Although there is little dispute regarding these large-scale paleogeographic elements a long-lasting and persistent controversy exists regarding the existence, provenance and pre-orogenic distribution of smaller terranes and oceanic basins that occupy the collision zone. Owing to the relatively small size of these elements, their existence cannot be tested by paleomagnetic or paleontological methods.
The granulite-gneiss extrusions in the Bohemian Massif are interpreted as parts of the lower plate, subducted, relaminated below the upper plate and exhumed as kilometre-scale translithospheric diapirs through upper plate. Because dominated by metagranites, it is repeatedly stated that they originated from continent subduction. Many studies were dedicated to their tectono-metamorphic Variscan evolution. Almost missing are studies trying to understand their paleo-environment that allowed such unprecedented travel of rocks through mantle.