Earth's mantle undergoes convection on million‐year timescales as heat is transferred from
depth to the surface. While this flow has long been linked to the large‐scale horizontal forces …

The existence of a thin, weak asthenospheric layer beneath Earth's lithospheric plates is
consistent with existing geological and geophysical constraints, including Pleistocene glacio …

SUMMARY During the Cenozoic, the Earth experienced multiple first-order geological
events that are likely mantle flow related. These include the termination of large-scale …

Australia undergoes a directional plate motion change from westward to northward motion in
the early Cenozoic that is associated with Australia/Antarctica separation. At the same time …

Interregional geological maps hold important information for geodynamic models. Here, we
use such maps to visualize major conformable and unconformable contacts at interregional …

Histories of large-scale horizontal and vertical lithosphere motion hold important information
on mantle convection. Here, we compare continent-scale hiatus maps as a proxy for mantle …

The tectonics of East Asia are notoriously complex. Consisting of an intricate patchwork of
microplates and accreted terranes, even the Cenozoic tectonic history of the region remains …

Geological maps are a powerful but underutilized tool for constraining geodynamic
processes and models. Unraveling the Cenozoic elevation history of Africa and …

Mantle convection is a fundamental process that shapes the Earth's surface by providing the
driving and resisting forces for horizontal motion of tectonic plates, as well as for inducing …

Mantle convection is a fundamental process in the Earth's system, yet its history remains
poorly known. Sophisticated inverse geodynamic Earth models are available to retrodict …