Add to ORKGThe 410 and 660 kmseismic discontinuities that bound the mantle transition zone (TZ) are attributed to phase transformations in olivine structure. This implies that variations in TZ thickness (HTZ) should correlate with those in TZ temperature. Pertinent seismic evidence has so far been ambiguous, however. We show that the transformations in olivine structure give rise to the 410 and 660 km discontinuities globally
We have investigated the complex spatial distribution of mineral phases in the Earth's upper mantle,...
cited By 18International audienceSeismic discontinuities at 410 and 660 km depth are usually attribu...
The 660-km seismic discontinuity (660) in Earth’s mantle is generally attributed to the breakdown of...
The 410 and 660 km seismic discontinuities that bound the mantle transition zone (TZ) are attributed...
The view that the seismic discontinuities bounding the mantle transition zone at 410- and 660-kilom...
The view that the seismic discontinuities bounding the mantle transition zone at 410- and 660-kilome...
We use a global data set of receiver functions to study the range of observations for the region at ...
182 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1999.An extrapolation of our data ...
The transition zone of Earth's mantle is delineated by globally observed discontinuities in seismic ...
The seismic discontinuities at depths near 400 and 650 km are primarily due to phase changes, but t...
The 660-km seismic discontinuity (660) in Earth’s mantle is generally attributed to the breakdown of...
The C-region of the upper mantle has two transition regions 75 to 90 kilometers thick. In western No...
The seismic discontinuities at 410 and 660 km depth in the mantle are generally believed to be due t...
Imposing a thermal and compositional significance to the outcome of the inversion of seismic data fa...
International audienceWe reassess the mantle transition zone structure below the northeast Asia marg...
We have investigated the complex spatial distribution of mineral phases in the Earth's upper mantle,...
cited By 18International audienceSeismic discontinuities at 410 and 660 km depth are usually attribu...
The 660-km seismic discontinuity (660) in Earth’s mantle is generally attributed to the breakdown of...
The 410 and 660 km seismic discontinuities that bound the mantle transition zone (TZ) are attributed...
The view that the seismic discontinuities bounding the mantle transition zone at 410- and 660-kilom...
The view that the seismic discontinuities bounding the mantle transition zone at 410- and 660-kilome...
We use a global data set of receiver functions to study the range of observations for the region at ...
182 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1999.An extrapolation of our data ...
The transition zone of Earth's mantle is delineated by globally observed discontinuities in seismic ...
The seismic discontinuities at depths near 400 and 650 km are primarily due to phase changes, but t...
The 660-km seismic discontinuity (660) in Earth’s mantle is generally attributed to the breakdown of...
The C-region of the upper mantle has two transition regions 75 to 90 kilometers thick. In western No...
The seismic discontinuities at 410 and 660 km depth in the mantle are generally believed to be due t...
Imposing a thermal and compositional significance to the outcome of the inversion of seismic data fa...
International audienceWe reassess the mantle transition zone structure below the northeast Asia marg...
We have investigated the complex spatial distribution of mineral phases in the Earth's upper mantle,...
cited By 18International audienceSeismic discontinuities at 410 and 660 km depth are usually attribu...
The 660-km seismic discontinuity (660) in Earth’s mantle is generally attributed to the breakdown of...