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Advanced filters: Author: Jacqueline E. Reber Clear advanced filters

Experimental demonstration of a semi-brittle origin for crustal strain transients

Plate tectonic motions cause faults to slip during earthquakes and through creep. Laboratory shear experiments on semi-brittle rock-analogue materials suggest that such slip could occur via growth of a series of fractures.

Jacqueline E. Reber
Luc L. Lavier
Nicholas W. Hayman
Research03 Aug 2015
Nature Geoscience

Volume: 8, P: 712-715
Repeated vaccination against matched H3N2 influenza virus gives less protection than single vaccination in ferrets

Nedzad Music
Wen-Pin Tzeng
Ian A. York
ResearchOpen Access09 Jul 2019
npj Vaccines

Volume: 4, P: 1-10

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Experimental demonstration of a semi-brittle origin for crustal strain transients

Repeated vaccination against matched H3N2 influenza virus gives less protection than single vaccination in ferrets

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