Abstract The Dora‐Maira massif is an archetypal nappe stack of subducted and exhumed
upper crust. Slices of continental crust experienced metamorphism at upper blueschist to …

Metamorphic timescales harbor crucial information for quantifying lithospheric processes
and identifying tectonic regimes. The Orosirian Period is known for global orogenesis during …

Exhumation rates for high-pressure metamorphic rocks need to be carefully estimated to
decipher tectonic processes in subduction/collision belts. In the Gran Paradiso Massif …

Exhumed high-pressure rocks formed during subduction provide insight into global
geodynamic and plate tectonic processes. Their metamorphic history is partially encoded in …

Plate tectonics is a key driver of many natural phenomena occurring on Earth, such as
mountain building, climate evolution and natural disasters. How plate tectonics has evolved …

The distribution of metamorphic rocks throughout the western European Alps indicates
subduction‐related metamorphism. However, processes by which high‐grade metamorphic …

Diapirism is crucial for heat and mass transfer in many geodynamic processes.
Understanding diapir ascent velocity is vital for assessing its significance in various …

The mechanisms attending the burial of crustal material and its exhumation before and
during the Alpine orogeny are controversial. New mechanical models propose local …

The Barrovian metamorphism of the Lepontine dome is manifested by isograds that cross‐
cut tectonic nappe contacts, which is commonly interpreted as metamorphism that occurred …

Pressure‐to‐depth conversion is a crucial step toward geodynamic reconstruction. The most
commonly used pressure‐to‐depth conversion method assumes that pressure corresponds …