According to GNSS/INSAR measurements, the Konya Basin in Central Anatolia is
undergoing rapid subsidence within an uplifting orogenic plateau. Further, geophysical …

Density instabilities in the lithosphere can founder gravitationally via viscous dripping and
decoupling from overlying crust. The lithospheric dripping concept has been invoked across …

The Cenozoic tectonic evolution of central Tibet plays an important role in the growth of the
Tibetan plateau. Paleoelevation studies show that the central Tibetan plateau hosted an …

Abstract The Central Andean Plateau is the largest plateau formed in a non-collisional
setting and is taller, wider, has thicker crust, and has greater retroarc shortening than any …

The basin and plateau regions of the Central Andes have undergone phases of rapid
subsidence and uplift during the last~ 20 Myr in addition to internal tectonic deformation …

Natural hydrogen is known to be generated in the crust by water/rock interactions, especially
the oxidation of iron-rich rock or radiolysis. However, other sources, especially deeper ones …

A long‐standing question is how felsic continental crust is differentiated from its mafic parent
mantle magmas. One currently proposed fundamental mechanism is lithospheric foundering …

Lithospheric foundering is an important mechanism of crustal deformation and recycling,
basin subsidence, and surface uplift in orogenic systems. The Arizaro Basin, in the Puna …

Amphibole exerts a fundamental control on arc magma petrogenesis, differentiation, and the
long-term evolution of the arc crust. This study identifies two texturally distinct amphibole …

Lithospheric foundering is hypothesized to contribute to the formation of Earth's largest
continental plateaus, but the predicted effects remain poorly constrained, especially …