Solid earth sciences

Iron snow, crystal floats, and inner-core growth: modes of core solidification and implications for dynamos in terrestrial planets and moons

Breuer D, Rueckriemen T, Spohn T

An in situ experimental study of Zr4+ transport capacity of water-rich fluids in the temperature and pressure range of the deep crust and upper mantle

Mysen B

Complex inner core boundary from frequency characteristics of the reflection coefficients of PKiKP waves observed by Hi-net

Tanaka S, Tkalčić H

Effect of width, amplitude, and position of a core mantle boundary hot spot on core convection and dynamo action

Dietrich W, Wicht J, Hori K

Can clay minerals account for the behavior of non-asperity on the subducting plate interface?

Katayama I, Kubo T, Sakuma H, Kawai K

Evidence for natural molecular hydrogen seepage associated with Carolina bays (surficial, ovoid depressions on the Atlantic Coastal Plain, Province of the USA)

Zgonnik V, Beaumont V, Deville E, Larin N, Pillot D, Farrrell K M

Geographical distribution of shear wave anisotropy within marine sediments in the northwestern Pacific

Tonegawa T, Fukao Y, Fujie G, Takemura S, Takahashi T, Kodaira S

Liquid Sodium Models of the Earth’s Core

Adams M M, Stone D R, Zimmerman D S, Lathrop D P

Towards more realistic core-mantle boundary heat flux patterns: a source of diversity in planetary dynamos

Amit H, Choblet G, Olson P, Monteux J, Deschamps F, Langlais B, Tobie G

Diffusion-controlled growth and degree of disequilibrium of garnet porphyroblasts: is diffusion-controlled growth of porphyroblasts common?

Miyazaki K