Results 191 to 200 of about 21,832 (251)

Hot versus cold subduction initiation. [PDF]

Natl Sci Rev
Li ZH.
europepmc   +1 more source

Seismic evidence for melt-rich lithosphere-asthenosphere boundary beneath young slab at Cascadia. [PDF]

Nat Commun
Wang X, Chen L, Wang K, Chen QF, Zhan Z, Yang J.   +5 more
europepmc   +1 more source

Wholesale flat subduction of the Indian slab and northward mantle convective flow: Plateau growth and driving force of the India-Asia collision. [PDF]

Proc Natl Acad Sci U S A
Ma J, Song X, Bunge HP, Fichtner A, Tian Y.   +4 more
europepmc   +1 more source

Western US intraplate deformation controlled by the complex lithospheric structure. [PDF]

Nat Commun
Cao Z, Liu L.
europepmc   +1 more source

Copper isotopes track the Neoproterozoic oxidation of cratonic mantle roots. [PDF]

Nat Commun
Chen C, Foley SF, Shcheka SS, Liu Y.
europepmc   +1 more source

Lithospheric models supported by the Caribbean and Levant examples help rethink transpression at plate boundaries. [PDF]

Nat Commun
Jourdon A, Le Pourhiet L, May DA, Pubellier M, Gabriel AA.   +4 more
europepmc   +1 more source

Dissecting the puzzle of tectonic lid regimes in terrestrial planets. [PDF]

Nat Commun
Lyu T, Ballmer MD, Li ZH, Lee MH, Yan J, Wu B, Zhao G.   +6 more
europepmc   +1 more source

Lunar hydrogen sources [PDF]

Okeefe, John A.
core   +1 more source

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Lateral Structural Variation of the Lithosphere‐Asthenosphere System in the Northeastern to Eastern Iranian Plateau and Its Tectonic Implications

Journal of Geophysical Research: Solid Earth, 2020
The Iranian plateau is a natural laboratory for deciphering the lithospheric deformation and deep dynamics in response to the Neo‐Tethyan subduction and subsequent Arabia‐Eurasia continental collision.
Z. Wu, Ling Chen, M. Talebian, Xu Wang, M. Jiang, Y. Ai, Haiqiang Lan, Yifan Gao, M. Khatib, Guangbing Hou, Sun‐Lin Chung, Xiaofeng Liang, Liang Zhao, Nasser Naimi-Ghassabian, W. Xiao, R. Zhu   +15 more
semanticscholar   +1 more source

The global asthenosphere

Izvestiya, Physics of the Solid Earth, 2011
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
openaire   +1 more source