Postseismic deformation due to subcrustal viscoelastic relaxation following dip-slip earthquakes [PDF]
The deformation of the Earth following a dip-slip earthquake is calculated using a three layer rheological model and finite element techniques. The three layers are an elastic upper lithosphere, a standard linear solid lower lithosphere, and a Maxwell ...
Cohen, S. C.
core +1 more source
Altimetry data and the elastic stress tensor of subduction zones [PDF]
The maximum shear stress (mss) field due to mass anomalies is estimated in the Apennines, the Kermadec-Tonga Trench, and the Rio Grande Rift areas and the results for each area are compared to observed seismicity.
Caputo, Michele
core +1 more source
Dual-layered mantle lithosphere beneath southeastern Canadian Cordillera. [PDF]
Nat CommunHuang S, Gu YJ, Johnston ST.
europepmc +1 more source
Himalayan sub-Moho earthquakes suggest crustal faults trigger eclogitized-drip tectonics. [PDF]
Sci RepSong X, Klemperer SL.
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Spreading modes at slow-spreading ridges shifted by mantle heterogeneity of the asthenosphere. [PDF]
Natl Sci RevZhang WQ +5 more
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Depth of slab breakoff in Archean: the role of radiogenic heat production of continental crust and eclogitization of oceanic crust. [PDF]
Sci RepFan YL, Zhang LF, Wang Y, Li ZH.
europepmc +1 more source
The importance of past rifting in large igneous province development. [PDF]
NatureKounoudis R +7 more
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Volcanism and long-term seismicity controlled by plume-induced plate thinning. [PDF]
Nat CommunBonadio R +5 more
europepmc +1 more source
Linking electrical anomalies in the upper mantle to petrological and geochemical heterogeneities. [PDF]
Natl Sci RevYang X, Xu YG, Xia QK.
europepmc +1 more source