Hugo van Schrojenstein Lantman

• PhD
• Postdoctoral Researcher at Utrecht University

The high‐pressure metamorphic Nevado‐Filábride Complex (NFC) in the Betics mountain range of southeastern Spain exhibits continental and ocean‐derived tectonic units, which are key for understanding the geodynamic evolution of the Western Mediterranean. We address the current debate in the definition of tectonic units, the emplacement of (ultra)maf...

The trace‐element composition of rutile is commonly used to constrain P‐T‐t‐conditions for a wide range of metamorphic systems. However, recent studies have demonstrated the redistribution of trace elements in rutile via high‐diffusivity pathways and dislocation‐impurity associations related to the formation and evolution of microstructures. Here w...

This study combines the microstructural and petrological analysis of garnet and its inclusions in quartzite‐hosted garnetite from the ultrahigh‐pressure Lago di Cignana metaophiolite (Western Alps). We present a comprehensive record of metamorphism, compaction, and the state of stress during interaction between oceanic metasediments and infiltratin...

With the recent recognition of Miocene subduction ages in the lower nappes of the Betic Cordillera, its tectonometamorphic evolution has become a point of discussion again. Neither of the two current models fully explains the metamorphic events found within the rocks of this domain, especially in the upper part of the downgoing plate. The metamorph...