TY - JOUR
T1 - Temperature dependence of [100](010) and [001](010) dislocation mobility in natural olivine
AU - Wang, Lin
AU - Blaha, Stephan
AU - Pintér, Zsanett
AU - Farla, Robert
AU - Kawazoe, Takaaki
AU - Miyajima, Nobuyoshi
AU - Michibayashi, Katsuyoshi
AU - Katsura, Tomoo
PY - 2016/5/1
Y1 - 2016/5/1
N2 - Dislocation recovery experiments were conducted on pre-deformed olivine single crystals at 1450 to 1760 K, room pressure, and oxygen partial pressures near the Ni–NiO buffer to determine the annihilation rates for [100] and [001] dislocations on the (010) plane. Olivine single crystals were first deformed to activate the desired slip systems under simple shear geometry and then annealed at target conditions. The edge and screw dislocations with Burgers vectors, b, of [100] and [001], respectively, both elongated in the [001] direction were produced by the deformation. The dislocation annihilation rate constants of both types of dislocations are identical within 0.3 log unit. The activation energies for both dislocations are also identical, i.e., ∼400 kJ/mol, which is also identical to that of the Si self-diffusion coefficient. This correspondence suggests that olivine dislocation creep controlled by a diffusion-controlled process under low-stress and high-temperature conditions. This study offers a potential insight into the formation of AG-type fabric in olivine.
AB - Dislocation recovery experiments were conducted on pre-deformed olivine single crystals at 1450 to 1760 K, room pressure, and oxygen partial pressures near the Ni–NiO buffer to determine the annihilation rates for [100] and [001] dislocations on the (010) plane. Olivine single crystals were first deformed to activate the desired slip systems under simple shear geometry and then annealed at target conditions. The edge and screw dislocations with Burgers vectors, b, of [100] and [001], respectively, both elongated in the [001] direction were produced by the deformation. The dislocation annihilation rate constants of both types of dislocations are identical within 0.3 log unit. The activation energies for both dislocations are also identical, i.e., ∼400 kJ/mol, which is also identical to that of the Si self-diffusion coefficient. This correspondence suggests that olivine dislocation creep controlled by a diffusion-controlled process under low-stress and high-temperature conditions. This study offers a potential insight into the formation of AG-type fabric in olivine.
KW - dislocation recovery
KW - olivine fabric
KW - seismic anisotropy
KW - slip system
KW - temperature dependence
UR - http://www.scopus.com/inward/record.url?scp=84978525019&partnerID=8YFLogxK
U2 - 10.1016/j.epsl.2016.02.029
DO - 10.1016/j.epsl.2016.02.029
M3 - Article
AN - SCOPUS:84978525019
SN - 0012-821X
VL - 441
SP - 81
EP - 90
JO - Earth and Planetary Science Letters
JF - Earth and Planetary Science Letters
ER -