Sentence examples for central mantle from inspiring English sources
While using them alone to identify individuals was problematic because standardized views of left and right sides were not available for direct comparison, they provided valuable supplemental information to the central mantle markings.
The lateral and central mantle and penetration area for every 5 degrees were also estimated.
Larvae express Ntu-Pax2/5/8 mainly bilaterally in two postero-ventral domains of the central mantle (Figs. 5 and 8a, b).
Most of this variation took place among the white markings on the central dorsal mantle rather than the consistent markings on the head, neck, and posterior tip of the mantle.
The death rate is high, the rate of recurrence higher still, and if that doesn't do it for you, consider the symbolic meaning of the heart, that central valentine in its mantle of muscle.
Instead, beneath the northeastern Japan arc, the subducted serpentinite along the slab undergoes dehydration and supplies fluids upward beneath the arc volcanic zones, causing melting in a high-temperature region of the central part of the mantle wedge (Iwamori 1998).
On a regional scale (i.e., hundreds of km in scale), the structure of the crust and the upper mantle in central Japan has been revealed by tomography studies (Nakajima and Hasegawa, 2007; Kamiya and Kobayashi, 2007).
Iidaka and Obara (1995) detected anisotropic regions in the mantle wedge beneath central Japan.
That heat led to the separation of the primordial body into a rocky crust, an underlying rocky mantle, and a central metallic core, hallmarks of planet Earth and the other rocky planets.
Iidaka and Obara (1995) studied seismic anisotropy in the mantle wedge in central Japan and found remarkable lateral variations: The magnitudes of shear-wave splitting time delays differed between the fore-arc and back-arc sides of the volcanic front, and the anisotropic region observed at the back-arc side of the volcanic front was characterized by low seismic velocity and low Q.
The switch of the bending direction of the isotherms in the mantle in the central model part from bend upwards (increasing geothermal gradient) to bend downwards (decreasing geothermal gradient) is thereby credited to the increasing depth of the LAB towards the south.
