Global plate motion models provide a spatial and temporal framework for geological data
and have been effective tools for exploring processes occurring at the earth's surface …

Following hundreds of millions of years of subduction in all circum-Pacific margins, the
Pacific Plate started to share a mid-ocean ridge connection with continental Antarctica …

Oceanic plateaus are mafic igneous provinces commonly thought to derive from ascending
mantle plumes. By far the largest, the Ontong Java Plateau (OJP) was emplaced ca. 120 Ma …

Seismic reflection profiles across the Hikurangi Plateau Large Igneous Province and
adjacent margins reveal the faulted volcanic basement and overlying Mesozoic‐Cenozoic …

The submarine volcanic emplacement of the Ontong Java Plateau (OJP) is the suggested
cause of Ocean Anoxic Event 1a (OAE 1a). However, no precise timing and duration exists …

The Andean Cordillera has evolved since the Late Cretaceous in the context of subduction
of oceanic lithosphere beneath continental lithosphere, making the kinematics between …

Here we present the first radiometric age data and a comprehensive geochemical data set
(including major and trace element and Sr–Nd–Pb–Hf isotope ratios) for samples from the …

We present a global community data set of fracture zones (FZs), discordant zones,
propagating ridges, V‐shaped structures and extinct ridges, digitized from vertical gravity …

We present 40Ar/39Ar age and geochemical (major and trace element and Sr–Nd–Hf–Pb
isotope) data from submarine samples recovered from the basement of the Manihiki Plateau …

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 …