[HTML][HTML] Coupled surface to deep Earth processes: Perspectives from TOPO-EUROPE with an emphasis on climate-and energy-related societal challenges
Understanding the interactions between surface and deep Earth processes is important for
research in many diverse scientific areas including climate, environment, energy …
research in many diverse scientific areas including climate, environment, energy …
The uplift of an early stage collisional plateau unraveled by fluvial network analysis and river longitudinal profile inversion: the case of the eastern Anatolian plateau
Orogenic plateaus of continental collision zones exhibit landforms and fluvial networks that
retain first-order information on their topographic evolution and vertical growth. The …
retain first-order information on their topographic evolution and vertical growth. The …
Post-delamination magmatism in south-central Anatolia
Quaternary mafic lavas in Central Anatolia provide geochemical insights into melt
generation processes following regional delamination of the subducted Tethyan slabs. New …
generation processes following regional delamination of the subducted Tethyan slabs. New …
Temporal and spatial variations in rock uplift from river‐profile inversions at the Central Anatolian Plateau southern margin
In geodynamically active areas, spatio‐temporal variations in rock uplift can provide key
insights into the processes responsible for the evolution of topography. The Central …
insights into the processes responsible for the evolution of topography. The Central …
Body‐wave tomographic imaging of the Turkana depression: Implications for rift development and plume‐lithosphere interactions
Abstract The Turkana Depression, a topographically subdued, broadly rifted zone between
the elevated East African and Ethiopian plateaus, disrupts the N–S, fault‐bounded rift basin …
the elevated East African and Ethiopian plateaus, disrupts the N–S, fault‐bounded rift basin …
The crustal structure of the Anatolian Plate from receiver functions and implications for the uplift of the central and eastern Anatolian plateaus
Understanding the crustal structure of the Anatolian Plate has important implications for its
formation and evolution, including the extent to which its high elevation is maintained …
formation and evolution, including the extent to which its high elevation is maintained …
Crustal melting and continent uplift by mafic underplating at convergent boundaries
The thick crust of the southern Tibetan and central Andean plateaus includes high-
conductivity, low-velocity zones ascribed to partial melt. The melt origin and effect on plateau …
conductivity, low-velocity zones ascribed to partial melt. The melt origin and effect on plateau …
High‐Resolution Broadband Lg Attenuation Structure of the Anatolian Crust and Its Implications for Mantle Upwelling and Plateau Uplift
Abstract The Anatolian Plateau, currently experiencing rapid uplift and westward escape,
records both the termination of oceanic subduction and the conversion to continental …
records both the termination of oceanic subduction and the conversion to continental …
Decoding stress patterns of the 2023 Türkiye‐Syria earthquake doublet
Earthquake interaction across multiple time scales can reveal complex stress evolution and
rupture patterns. Here, we investigate the role of static stress change in the 2023 Mw 7.8 and …
rupture patterns. Here, we investigate the role of static stress change in the 2023 Mw 7.8 and …
When did the Dead Sea fault become a transform?
This study re-evaluates the∼ 20 Myr development of the Dead Sea Fault System (DSFS)
and its tectonic definition as a transform plate boundary. The DSFS conveys sinistral …
and its tectonic definition as a transform plate boundary. The DSFS conveys sinistral …