Depletion of the upper mantle by convergent tectonics in the Early Earth [PDF]
Scientific Reports, 2021 Partial melting of mantle peridotites at spreading ridges is a continuous global process that forms the oceanic crust and refractory, positively buoyant residues (melt-depleted mantle peridotites).
A. L. Perchuk +3 more
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High-pressure elastic properties of dolomite melt supporting carbonate-induced melting in deep upper mantle [PDF]
Proceedings of the National Academy of Sciences of the United States of America, 2020 Man Xu, Zhicheng Jing, Suraj K Bajgain
exaly +2 more sources
Speed structure of the mantle of the border of the Eastern European and West European platforms
Геофизический журнал, 2021 This work is devoted to studying the velocity structure of the mantle of the border area of the East European and West European platforms in the crust separated by the Teiserre-Tornquist zone.
T. A. Tsvetkova +2 more
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Seismological reference earth model in South China (SREM-SC): Upper mantle
Frontiers in Earth Science, 2023 This work is the mantle component of constructing the Seismological Reference Earth Model in South China (SREM-SC). Although there has been a wide range of research for imaging the upper mantle structures beneath South China, most of them focus on the ...
Qingya Tang +5 more
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Water in the upper mantle and deep crust of eastern China: concentration, distribution and implications [PDF]
National Science Review, 2019 Qun-Ke Xia, Jia Liu, István Kovacs
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Геодинамика и тектонофизика, 2021 A geodynamic model of upper mantle convection related to the Pacific subduction zone is mathematically substantiated and applied to investigate the Cretaceous-Cenozoic evolution of Central East Asia (CEA) and the Arctic. We present a solution for the two-
L. I. Lobkovsky +2 more
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Upper-plate Shortening and Mountain-building in the Context of Mantle-driven Oceanic Subduction
Tektonika, 2023 The mechanisms controlling mountain building at subduction zones remain debated. In particular the interaction between mantle flow and subduction has been poorly addressed while fundamental in controlling plate displacement and deformation.
Tania Habel +5 more
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Low‐Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation
Geophysical Research Letters, 2023 The upper mantle is heterogeneous in Fe isotope compositions, but the origin of the heterogeneity needs understanding. Recent studies on oceanic basalts demonstrate that the upper mantle Fe isotope heterogeneity results from low‐degree melt metasomatism.
Pengyuan Guo +7 more
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Upper Mantle Anisotropy and Flow Beneath the Pacific Ocean Revealed by Differential PS‐SKS Splitting
Geophysical Research Letters, 2023 Upper mantle anisotropy has been mapped beneath continents at high spatial resolution. Beneath the oceans, however, shear wave splitting constraints on upper mantle anisotropy are sparse, due to the paucity of seismic receivers. A technique that does not
Jonathan Wolf, Maureen D. Long
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Effects of Composite Rheology on Plate‐Like Behavior in Global‐Scale Mantle Convection
Geophysical Research Letters, 2023 Earth's upper mantle rheology controls lithosphere‐asthenosphere coupling and thus surface tectonics. Rock deformation experiments and seismic anisotropy measurements indicate that composite rheology (co‐existing diffusion and dislocation creep) occurs ...
Maëlis Arnould +2 more
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