Sensitivity of teleseismic body waves to mineral texture and melt in the mantle beneath a mid–ocean ridge
Author:
Affiliation:
1. Department of Earth Sciences, University of Leeds, Leeds LS2 9JT, UK
Publisher
The Royal Society
Subject
General Physics and Astronomy,General Engineering,General Mathematics
Link
https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.1997.0007
Reference54 articles.
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2. Recording teleseismic earthquakes using ocean bottom seismographs at mid-ocean ridges;Blackman D. K.;Bull. Seism. Soc. Am.,1995
3. Blackman D. K. Kendall J.-M. Dawson P. R. Wenk H.-R. Boyce D. & Phipps Morgan J. 1997 Teleseismic imaging of subaxial flow at mid-ocean ridges: travel time effects of anisotropic mineral texture in the mantle. Geophys. J. Int. (In the press.)
4. Ceuleneer G. & Rabinowicz M. 1992 Mantle flow and melt migration beneath oceanic ridges: models derived from observations in ophiolites. In Mantle flow and melt generation at midocean ridges (ed. J. Phipps Morgan et al.) pp. 123-154. (Geophysical Monograph 71.) Washington DC: AGU.
5. Thermal structure of a fossil mantle diapir inferred from the distribution of mafic cumulates
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