The Urey ratio describes the contribution of internal heat production to planetary‐scale
energy balance, and knowing this thermal budget for Earth is essential to understand its …

Hot spot–mid‐ocean ridge interactions cause many of the largest structural and chemical
anomalies in Earth's ocean basins. Correlated geophysical and geochemical anomalies are …

The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …

The onset of partial melting beneath mid-ocean ridges governs the cycling of highly
incompatible elements from the mantle to the crust, the flux of key volatiles (such as CO2, He …

Partial melts in the Earth's convecting mantle influence its physical and chemical state,
particularly the plasticity of the asthenosphere and the dynamics of plate tectonics. Melt …

Plate tectonic theory was developed 50 years ago and underpins most of our understanding
of Earth's evolution. The theory explains observations of magnetic lineations on the seafloor …

Presenting a coherent synthesis of lithosphere studies, this book covers a range of
geophysical methods (seismic reflection, refraction, and receiver function methods; elastic …

The speciation of carbon in the Earth's mantle is largely governed by oxygen fugacity. Under
reducing conditions carbon forms graphite, diamond or CH4, while under more oxidising …

We review and describe the electromagnetic transmitters and receivers used to carry out
magnetotelluric and controlled source soundings in the marine environment. Academic …

Abstract Knowledge of the occurrence and mobility of carbonate-rich melts in the Earth's
mantle is important for understanding the deep carbon cycle and related geochemical and …