Western US intraplate deformation controlled by the complex lithospheric structure. [PDF]
Nat CommunCao Z, Liu L.
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Copper isotopes track the Neoproterozoic oxidation of cratonic mantle roots. [PDF]
Nat CommunChen C, Foley SF, Shcheka SS, Liu Y.
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Lithospheric models supported by the Caribbean and Levant examples help rethink transpression at plate boundaries. [PDF]
Nat CommunJourdon A +4 more
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Coevolution of craton margins and interiors during continental break-up. [PDF]
NatureGernon TM +7 more
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Channelized metasomatism in Archean cratonic roots as a mechanism of lithospheric refertilization. [PDF]
Nat CommunRoots EA +6 more
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Dissecting the puzzle of tectonic lid regimes in terrestrial planets. [PDF]
Nat CommunLyu T +6 more
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New geochemical and Sr-Nd-Hf isotopic constraints on the genesis of kimberlites and ultramafic lamprophyres from the Adelaide Fold Belt and Gawler Craton, South Australia. [PDF]
Mineral PetrolDalton H +3 more
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Based on the analysis of the thermal history of the mantle, we hypothesize the existence of the partially molten layer at a depth of approximately 700–1100 km under the entire Earth's surface. We present the seismological data that are consistent with this hypothesis and the geoelectric results revealing the conductive layer at similar depths in ...
V. V. Gordienko, I. M. Logvinov
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The Lithosphere-Asthenosphere Boundary
Annual Review of Earth and Planetary Sciences, 2010Seismological models of upper-mantle structure are providing new constraints on the physical and chemical properties that differentiate the lithosphere from the asthenosphere. A wide variety of studies are consistent with an oceanic lithosphere that corresponds to a dry, chemically depleted layer over a hydrated, fertile asthenosphere.
Fischer, Karen M. +3 more
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