Depletion of the upper mantle by convergent tectonics in the Early Earth [PDF]
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
doaj +2 more sources
Water in the upper mantle and deep crust of eastern China: concentration, distribution and implications [PDF]
Understanding the concentration and distribution of water in the Earth's mantle plays a substantial role in studying its chemical, physical and dynamic processes.
Qun-Ke Xia, Jia Liu, Istvan Kovacs
exaly +3 more sources
Abiotic polycyclic aromatic hydrocarbons originating from the sub-oceanic mantle [PDF]
Experimental studies have demonstrated that petroleum may form from abiotic organic compounds synthesised in the Earth’s upper mantle. However, the most direct evidence of mantle-derived organics, as obtained from whole-rock analyses, indicates ambiguous
Itaru Mitsukawa +13 more
doaj +2 more sources
High-pressure elastic properties of dolomite melt supporting carbonate-induced melting in deep upper mantle [PDF]
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
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
doaj +1 more source
Seismological reference earth model in South China (SREM-SC): Upper mantle
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
doaj +1 more source
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
doaj +1 more source
Upper-plate Shortening and Mountain-building in the Context of Mantle-driven Oceanic Subduction
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
doaj +1 more source
Low‐Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation
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
doaj +1 more source
Upper Mantle Anisotropy and Flow Beneath the Pacific Ocean Revealed by Differential PS‐SKS Splitting
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
doaj +1 more source

