In the last 20 years, one of the biggest discovery in seismology is probably the discovery of slow earthquakes. Slow earthquakes are called slow because, contrary to regular earthquakes, they poorly radiate any seismic waves. Slow slip phenomenas have been classified in different kinds of events, all of them related to each other but different. I am particularly focus on the detection of one of them called tremors.

Related articles:

• Romanet, P. and Ide, S., 2019. Ambient tectonic tremors in Manawatu, Cape Turnagain, Marlborough, and Puysegur, New Zealand. Earth, Planets and Space, 71(1), p.59.
• Romanet, P., Bhat, H.S., Jolivet, R. and Madariaga, R., 2018. Fast and slow slip events emerge due to fault geometrical complexity. Geophysical Research Letters, 45(10), pp.4809-4819.