Modeling the seismic signature of structural data from the Oman Ophiolite: Can a mantle diapir be detected beneath the East Pacific Rise?
- DOI
- 10.1029/2002gc000418
- Published
- 2003-07
- Container
- Geochemistry, Geophysics, Geosystems
- Publisher
- American Geophysical Union (AGU)
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1029/2002gc000418,
title = {Modeling the seismic signature of structural data from the Oman Ophiolite: Can a mantle diapir be detected beneath the East Pacific Rise?},
author = {David Jousselin and Robert Dunn and Douglas R. Toomey},
year = {2003},
journal = {Geochemistry, Geophysics, Geosystems},
doi = {10.1029/2002gc000418},
url = {https://doi.org/10.1029/2002gc000418}
}RIS
TY - JOUR TI - Modeling the seismic signature of structural data from the Oman Ophiolite: Can a mantle diapir be detected beneath the East Pacific Rise? AU - David Jousselin AU - Robert Dunn AU - Douglas R. Toomey PY - 2003 JO - Geochemistry, Geophysics, Geosystems DO - 10.1029/2002gc000418 UR - https://doi.org/10.1029/2002gc000418 ER -
APA
Jousselin, D., Dunn, R., & Toomey, D. R. (2003). Modeling the seismic signature of structural data from the Oman Ophiolite: Can a mantle diapir be detected beneath the East Pacific Rise?. Geochemistry, Geophysics, Geosystems. https://doi.org/10.1029/2002gc000418
Source records
- crossref · retrieved 2026-09-26T09:09:16.409Z