A transformative advance in Earth science is the development of low‐temperature
thermochronometry to date Earth surface processes or quantify the thermal evolution of …

The internal zones of the Western Alps arc are derived from an oceanic and continental
subduction wedge developed beneath the Adria plate during its paleogene northward drift …

Minerals on fault surfaces record fluid-rock interaction, strain, and/or heat during fault slip.
Fault-hosted hematite is amenable to (U–Th)/He (He) thermochronometry. Hematite He …

This paper presents a novel, cost-effective method for a rapid and quantitative
characterization of discontinuities in fractured rock cliffs using Unmanned Aerial Vehicle …

The~ 2,000-km-long Central Range of New Guinea is a hotspot of modern carbon
sequestration due to the chemical weathering of igneous rocks with steep topography in the …

Abstract In the Internal Zone of a continental collisional orogen, first-order contractional
shear zones accommodate crustal shortening. Structural investigations at different scales …

Foreland basin sedimentary strata are key records of orogenic development, but identifying
detrital thermochronometers of appropriate temperature sensitivity to detect provenance …

The present research explores a diverse suite of soft sediment deformation structures
(SSDS) combined with clastic dykes and shear deformation bands distributed throughout a …

The Variscan high‐grade metamorphic basement of northern Sardinia and southern Corsica
record lower Carboniferous anatexis related to post‐collisional decompression of the …

We report the first description of a~ 15 km long NE-SW-striking transtensive fault network
crosscutting the metamorphic units of the Ligurian Alps. The main fault zone, hereby named …