Rachel Abercrombie
Affiliations: | Boston University, Boston, MA, United States |
Area:
Geophysics, Plate TectonicsGoogle:
"Rachel Abercrombie"Mean distance: (not calculated yet)
Children
Sign in to add trainee| Gisela S. Magalhaes de Matos Viegas Fernandes | grad student | 2010 | Boston University |
BETA: Related publications
See more...
Publications
|
You can help our author matching system! If you notice any publications incorrectly attributed to this author, please sign in and mark matches as correct or incorrect. |
| Kammer DS, McLaskey GC, Abercrombie RE, et al. (2024) Earthquake energy dissipation in a fracture mechanics framework. Nature Communications. 15: 4736 |
| Wang QY, Frank WB, Abercrombie RE, et al. (2023) What makes low-frequency earthquakes low frequency. Science Advances. 9: eadh3688 |
| Abercrombie RE. (2021) Resolution and uncertainties in estimates of earthquake stress drop and energy release. Philosophical Transactions. Series a, Mathematical, Physical, and Engineering Sciences. 379: 20200131 |
| Abercrombie RE. (2019) Small and large earthquakes can have similar starts. Nature. 573: 42-43 |
| Prieto GA, Froment B, Yu C, et al. (2017) Earthquake rupture below the brittle-ductile transition in continental lithospheric mantle. Science Advances. 3: e1602642 |
| Abercrombie R. (2005) Seismology: the start of something big? Nature. 438: 171-3 |
| Ellsworth B, Ito H, Malin P, et al. (2001) In Jules Verne's Footsteps: Seismology in the source Eos, Transactions American Geophysical Union. 82: 333-339 |
| Gledhill K, Robinson R, Webb T, et al. (2000) The MW 6.2 Cass, New Zealand, earthquake of 24 November 1995: Reverse faulting in a strike‐slip region New Zealand Journal of Geology and Geophysics. 43: 255-269 |
| Leary P, Abercrombie R. (1994) Fractal fracture scattering origin of S-wave coda : spectral evidence from recordings at 2.5 Km Geophysical Research Letters. 21: 1683-1686 |
| Leary P, Abercrombie R. (1994) Frequency dependent crustal scattering and absorption at 5–160 Hz from coda decay observed at 2.5 km Depth Geophysical Research Letters. 21: 971-974 |