Ridge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years ago
A reorganization centered on the Pacific plate occurred~ 53–47 million years ago. A “top‐
down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a …
down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a …
A geodynamic and mineral physics model of a solid-state ultralow-velocity zone
Recent results (Wicks et al., 2010) suggest that a mixture of iron-enriched (Mg, Fe) O and
ambient mantle is consistent with wavespeed reductions and density increases inferred for …
ambient mantle is consistent with wavespeed reductions and density increases inferred for …
The GPlates geological information model and markup language
X Qin, RD Müller, J Cannon… - … , Methods and Data …, 2012 - gi.copernicus.org
Understanding tectonic and geodynamic processes leading to the present-day configuration
of the Earth involves studying data and models across a variety of disciplines, from …
of the Earth involves studying data and models across a variety of disciplines, from …
Enhanced convection and fast plumes in the lower mantle induced by the spin transition in ferropericlase
Using a numerical model we explore the consequences of the intrinsic density change
(Δρ/ρ≈ 2–4%) caused by the Fe2+ spin transition in ferropericlase on the style and vigor of …
(Δρ/ρ≈ 2–4%) caused by the Fe2+ spin transition in ferropericlase on the style and vigor of …
Dynamic origins of seismic wavespeed variation in D ″
The D ″discontinuity is defined by a seismic velocity increase of 1–3% about 250km above
the core–mantle boundary (CMB), and is mainly detected beneath locations of inferred …
the core–mantle boundary (CMB), and is mainly detected beneath locations of inferred …
[BOOK][B] Geodynamics of Earth's Deep Mantle
DJ Bower - 2012 - search.proquest.com
Seismic tomography and waveform modeling reveal several prominent structures in the
Earth's lower mantle:(1) the D''discontinuity, defined by a seismic velocity increase of 1–3 …
Earth's lower mantle:(1) the D''discontinuity, defined by a seismic velocity increase of 1–3 …
[CITATION][C] 地球深部科学研究的新进展--记 2007 年美国地球物理联合会 (AGU)
赵素涛, 金振民 - 地学前缘, 2008