Abstract The Central and Eastern Anatolian plateaus are integral parts of the world's third
largest orogenic plateau. In the past decade, geophysical surveys have provided insights …

The driving force for transient vertical motions of Earth's surface remains an outstanding
question. A main difficulty lies in the uncertain role of the underlying mantle, especially …

The origin and tectonic setting of the Mesoproterozoic (1.50–1.34 Ga) granite–rhyolite
Provinces of the midcontinent region of the United States, and the coeval A-type granite …

Rayleigh wave phase velocity maps from ambient noise and earthquake data are inverted
jointly with receiver functions observed at 828 stations from the USArray Transportable Array …

Conventional wisdom holds that the southern Appalachian Mountains have not experienced
a significant phase of tectonic forcing for> 200 myr; yet, they share many characteristics with …

Abstract Late Cenozoic (and especially Quaternary) fluvial deposits and related landforms
provide valuable information about landscape evolution, not just in terms of changing …

Seismic structure beneath the contiguous US was imaged with multimode receiver function
stacking and inversion of Rayleigh wave dispersion and ellipticity measurements. Crust …

We apply a novel 3‐D multiobservable probabilistic tomography method that we have
recently developed and benchmarked, to directly image the thermochemical structure of the …

ABSTRACT Rainfall on 9–13 September 2013 triggered at least 1,138 debris flows in a
3430 km2 area of the Colorado Front Range. The historical record reveals that the …

The history of erosion of southwestern North America and its relationship to surface uplift is a
long-standing topic of debate. We use geologic and thermochronometric data to reconstruct …