Continental lithosphere is deformed, destroyed, or otherwise modified in several ways.
Processes that modify the lithosphere include subduction, terrane accretion, orogenesis …

ABSTRACT Auckland Volcanic Field (AVF) is a basaltic intraplate volcanic field in North
Island, New Zealand, upon which> 1.6 million people live. Seismic velocity tomography and …

Cratonic lithospheric mantle is composed of predominantly refractory materials that formed
at higher mantle potential temperatures (TP) than recorded in non-cratonic peridotites. It also …

Abstract The Cenozoic East African rift (EAR), Cameroon Volcanic Line (CVL), and Atlas
Mountains formed on the slow‐moving African continent, which last experienced orogeny …

Abstract Preceding the early Toarcian Oceanic Anoxic Event by∼ 1 Myr, the Pliensbachian–
Toarcian boundary event is in many aspects as severe and disturbing for the environment as …

We compiled geochronology data from 87 published studies within the Anatolia orogen
(32.5 E–44 E) to investigate the spatial and temporal patterns of continental magmatism …

Geophysically detectible mid-lithospheric discontinuities (MLD) and lithosphere-
asthenosphere boundaries (LAB) beneath cratons have received much attention over recent …

After the onset of continental collision, magmatism often persists for tens of millions of years,
albeit with a different composition, in reduced volumes, and with a more episodic nature and …

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 …

Several of Earth's intraplate volcanic provinces are hard to reconcile with the mantle plume
hypothesis. Instead, they exhibit characteristics that are more compatible with shallower …