Over 50% of Earth is covered by oceanic crust, the uppermost portion of which is a high-
permeability layer of basaltic lavas through which seawater continuously circulates. Fluid …

Abstract Intraplate Continental Margins comprise fully rifted areas of continents and cratons
recording the tectonic events associated with plate breakup and subsequent continental …

In this paper, we use a robust inversion algorithm, which we have tested in many regional
studies, to obtain the first global model of Curie-point depth (GCDM) from magnetic anomaly …

The existence of stabilizing feedbacks within Earth's climate system is generally thought to
be necessary for the persistence of liquid water and life. Over the course of Earth's history …

Over the last decade, seismological studies have shed new light on the properties of the
mantle lithosphere and their physical and chemical origins. This paper synthesizes recent …

Marine transform faults and associated fracture zones (MTFFZs) cover vast stretches of the
ocean floor, where they play a key role in plate tectonics, accommodating the lateral …

Abstract The Eastern and Southeastern Asian regions witness the strongest land–ocean and
lithosphere–asthenosphere interactions. The extreme diversity of geological features …

Topography and bathymetry are principally supported by some combination of crustal and
sub‐crustal density variations. However, dynamic topography is generated by vertical …

We present three‐dimensional simulations of coupled fluid and heat transport in the ocean
crust, to explore patterns and controls on ridge‐flank hydrothermal circulation on the eastern …

Peak heat flow occurs at mid-ocean ridges and decreases with the age of the oceanic
lithosphere. Several plate models, including the Parsons and Sclater (PSM) model, Global …