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Crustal anatomy and evolution of a subduction-related orogenic system: Insights from the Southern Central Andes (22-35 S)
As the archetype of mountain building in subduction zones, the Central Andes has
constituted an excellent example for investigating mountain-building processes for decades …
constituted an excellent example for investigating mountain-building processes for decades …
The Atlas of Morocco: A plume‐assisted orogeny
We explore the connections between crustal shortening, volcanism, and mantle dynamics in
the Atlas of Morocco. In response to compressional forces and strain localization, this …
the Atlas of Morocco. In response to compressional forces and strain localization, this …
Formation of continental microplates through rift linkage: Numerical modeling and its application to the Flemish Cap and Sao Paulo Plateau
Continental microplates are enigmatic plate boundary features, which can occur in
extensional and compressional regimes. Here we focus on microplate formation and their …
extensional and compressional regimes. Here we focus on microplate formation and their …
Bridging the gap between experimental and natural fabrics: Modeling ice stream fabric evolution and its comparison with ice‐core data
Fabrics, also known as textures or crystallographic preferred orientations, reveal information
about the deformation history of the flow of polycrystalline materials, including glacial ice …
about the deformation history of the flow of polycrystalline materials, including glacial ice …
Lithospheric structure of the Malawi Rift: Implications for magma‐poor rifting processes
Our understanding of how magma‐poor rifts accommodate strain remains limited largely
due to sparse geophysical observations from these rift systems. To better understand the …
due to sparse geophysical observations from these rift systems. To better understand the …
Evolving subduction zone thermal structure drives extensive forearc mantle wedge hydration
Hydration of the subduction zone forearc mantle wedge influences the downdip distribution
of seismicity, the availability of fluids for arc magmatism, and Earth's long term water cycle …
of seismicity, the availability of fluids for arc magmatism, and Earth's long term water cycle …
Subduction without volcanic arc magma: Insights from two young subduction zones in the western Pacific
Missing volcanic arcs in young subduction zones are commonly attributed to an insufficient
subduction depth of the downgoing slab. The North Sulawesi subduction zone (NSS) in the …
subduction depth of the downgoing slab. The North Sulawesi subduction zone (NSS) in the …
Modeling viscoelastic solid earth deformation due to ice age and contemporary glacial mass changes in ASPECT
The redistribution of past and present ice and ocean loading on Earth's surface causes solid
Earth deformation and geoid changes, known as glacial isostatic adjustment. The …
Earth deformation and geoid changes, known as glacial isostatic adjustment. The …
Crustal flow driving twin domes exhumation and low-angle normal faulting in the Menderes Massif of western Anatolia
Lower crustal flow in regions of post-orogenic extension has been inferred to explain the
exhumation of metamorphic core complexes and associated low-angle normal (detachment) …
exhumation of metamorphic core complexes and associated low-angle normal (detachment) …
Hindered trench migration due to slab steepening controls the formation of the Central Andes
The formation of the Central Andes dates back to∼ 50 Ma, but its most pronounced episode,
including the growth of the Altiplano‐Puna Plateau and pulsatile tectonic shortening phases …
including the growth of the Altiplano‐Puna Plateau and pulsatile tectonic shortening phases …