Sublithospheric diamonds and the inclusions they may carry crystallize in the
asthenosphere, transition zone, or uppermost lower mantle (from 300 to∼ 800 km), and are …

Sonification uses non-speech audio to convey complex data patterns in both space and
time, overcoming visual and language barriers to science communication. Data sonification …

Oceanic anoxic events are geologically abrupt phases of extreme oxygen depletion in the
oceans that disrupted marine ecosystems and brought about evolutionary turnover. Typically …

Argyle is the world's largest source of natural diamonds, yet one of only a few economic
deposits hosted in a Paleoproterozoic orogen. The geodynamic triggers responsible for its …

Many cratonic continental fragments dispersed during the rifting and break-up of Gondwana
are bound by steep topographic landforms known as 'great escarpments',,–, which rim …

Abstract The South American Platform encompasses the São Francisco Craton (SFC) and
the Araçuaí-Ribeira orogenic system (AROS) located in the eastern Brazil. These geologic …

The mid-Archean to mid-Proterozoic appears to have favored the formation of cratons, stable
crustal shields underlain by unusually thick and cold mantle roots. Most of these cratons and …

Earth's tectonic history is punctuated by several cycles of supercontinent assembly and
breakup that profoundly influenced the lithospheric structure; however, the roles of the …

A diffuse magmatic province covering central‐eastern Asia continent displays a
compositional transition at 120–100 Ma and probably reflects melting initiation in isotopically …

Whether the supercontinent cycle (Sc) is the major process driving plate tectonics evolution
has not been purposely investigated. If true, it would result in more geological records …