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Nicolaas Jacob Vlaar grad student 1976 Utrecht
 (Higher modes and the determination of upper mantle structure.)


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Wim Spakman grad student 1988 Utrecht
Sergei A. Lebedev grad student 2000 Princeton (Physics Tree)
Raffaella Montelli grad student 2003 Princeton (Physics Tree)
Karin Sigloch grad student 2008 Princeton (Physics Tree)
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Nolet G, Hello Y, Lee SV, et al. (2019) Imaging the Galápagos mantle plume with an unconventional application of floating seismometers. Scientific Reports. 9: 1326
Sukhovich A, Bonnieux S, Hello Y, et al. (2015) Seismic monitoring in the oceans by autonomous floats. Nature Communications. 6: 8027
Joubert C, Nolet G, Sukhovich A, et al. (2015) Hydrophone calibration at very low frequencies Bulletin of the Seismological Society of America. 105: 1797-1802
Voronin S, Mikesell D, Nolet G. (2015) Compression approaches for the regularized solutions of linear systems from large-scale inverse problems Gem - International Journal On Geomathematics. 6: 251-294
Nolet G. (2015) Transmission tomography in seismology Handbook of Geomathematics: Second Edition. 1887-1904
Marot M, Monfret T, Gerbault M, et al. (2014) Flat versus normal subduction zones: A comparison based on 3-D regional traveltime tomography and petrological modelling of central Chile and western Argentina (29°-35°S) Geophysical Journal International. 199: 1633-1654
Voronin S, Mikesell D, Slezak I, et al. (2014) Solving large tomographic linear systems: Size reduction and error estimation Geophysical Journal International. 199: 276-285
Bonnin M, Nolet G, Villaseñor A, et al. (2014) Multiple-frequency tomography of the upper mantle beneath the African/Iberian collision zone Geophysical Journal International. 198: 1458-1473
Sukhovich A, Irisson JO, Perrot J, et al. (2014) Automatic recognition of T and teleseismic P waves by statistical analysis of their spectra: An application to continuous records ofmoored hydrophones Journal of Geophysical Research B: Solid Earth. 119: 6469-6485
Zaroli C, Sambridge M, Lévêque JJ, et al. (2013) An objective rationale for the choice of regularisation parameter with application to global multiple-frequency S-wave tomography Solid Earth. 4: 357-371
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