Synchronization of chaos refers to a process wherein two (or many) chaotic systems (either
equivalent or nonequivalent) adjust a given property of their motion to a common behavior …

Hydrothermal circulation and alteration at mid-ocean ridges and ridge flanks have a key role
in regulating seawater chemistry and global chemical fluxes, and support diverse …

The oxygen isotope compositions of carbonate and phosphatic fossils hold the key to
understanding Earth-system evolution during the last 500 million years. Unfortunately, the …

The number of heat flow measurements at the Earth surface has significantly increased
since the last global analysis (Pollack et al., 1993, https://doi. org/10.1029/93RG01249), and …

This enduringly popular undergraduate textbook has been thoroughly reworked and
updated, and now comprises twelve chapters covering the same breadth of topics as earlier …

Without deep mixing, the ocean would turn, within a few thousand years, into a stagnant
pool of cold salty water with equilibrium maintained locally by near-surface mixing and with …

A global map of surface heat flow is presented on a 2°× 2° equal area grid. It is based on a
global heat flow data set of over 38,000 measurements. The map consists of three …

Porphyry deposits arguably represent the most economically important class of nonferrous
metallic mineral resources. These magmatic-hydrothermal deposits are characterized by …

Theory of the Earth is an interdisciplinary advanced textbook on the origin, composition, and
evolution of the Earth's interior: geophysics, geochemistry, dynamics, convection …

▪ Abstract Geophysical estimates of mid-ocean ridge axial heat fluxes (2–4× 1012 W) and of
the total hydrothermal flux (9±2× 1012 W) are well established. Problems arise in calculation …