Solid earth sciences

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

Katayama I, Kubo T, Sakuma H, Kawai K

Abstracts

SpringerOpen

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

Abstracts

SpringerOpen

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

Abstracts

SpringerOpen

Liquid Sodium Models of the Earth’s Core

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

Abstracts

SpringerOpen

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

Abstracts

SpringerOpen

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

Miyazaki K

Abstracts

SpringerOpen

The competition between Lorentz and Coriolis forces in planetary dynamos

Soderlund K M, Sheyko A, King E M, Aurnou J M

Abstracts

SpringerOpen

Water and magmas: insights about the water solution mechanisms in alkali silicate melts from infrared, Raman, and 29 Si solid-state NMR spectroscopies

Le Losq C, Mysen B O, Cody G D

Abstracts

SpringerOpen

Historical and paleo-tsunami deposits during the last 4000 years and their correlations with historical tsunami events in Koyadori on the Sanriku Coast, northeastern Japan

Ishimura D, Miyauchi T

Abstracts

SpringerOpen

Stratification of Earth's outermost core inferred from SmKS array data

Kaneshima S, Matsuzawa T

Abstracts

SpringerOpen