Imaging Lithospheric Discontinuities Beneath the Northern East African Rift Using S-to-P Receiver Functions. [PDF]
Lavayssière A +7 more
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Analysis of the b, p values, and the fractal dimension of aftershocks sequences following two major earthquakes in central Himalaya. [PDF]
Tiwari RK, Paudyal H.
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Adaptive Evolution of Nearctic Deepwater Fish Vision: Implications for Assessing Functional Variation for Conservation. [PDF]
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Actively forming microbial mats provide insight into the development of microdigitate stromatolites. [PDF]
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Crustal melting and continent uplift by mafic underplating at convergent boundaries. [PDF]
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Characterization of a Thermostable Endolysin of the Aeribacillus Phage AeriP45 as a Potential Staphylococcus Biofilm-Removing Agent. [PDF]
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Rifting Attractor Structures in the Baikal Rift System: Location and Effects
Journal of Asian Earth Sciences, 2014Abstract The current geodynamics and tectonophysics of the Baikal rift system (BRS) as recorded in lithospheric stress and strain are discussed in the context of self organization of nonlinear dissipative dynamic systems and nonlinear media. The regional strain field inferred from instrumental seismic moment and fault radius data for almost 70,000 M
Anatoly Klyuchevskii
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Baikal Rift: Active or Passive? — Comparison of the Baikal and Kenya Rift Zones
Tectonophysics, 1983Abstract The comparison of geological and geophysical data from the Kenya and Baikal rift zones permits us to consider the formation of these zones to be associated with the development of wide asthenospheric upwellings beneath them. In this sense, both rifts are active.
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