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The seismic anomaly beneath Iceland extends down to the mantle transition zone and no deeper (2000)
Journal Article
Foulger, G., Pritchard, M., Julian, B., Evans, J., Allen, R., Nolet, G., …Vogfjord, K. (2000). The seismic anomaly beneath Iceland extends down to the mantle transition zone and no deeper. Geophysical Journal International, 142, F1-F5. https://doi.org/10.1046/j.1365-246x.2000.00245.x

A 3-D teleseismic tomography image of the upper mantle beneath Iceland of unprecedented resolution reveals a subvertical low wave speed anomaly that is cylindrical in the upper 250 km but tabular below this. Such a morphological transition is expecte... Read More about The seismic anomaly beneath Iceland extends down to the mantle transition zone and no deeper.

Geological framework of Britain and Ireland. (2000)
Book Chapter
Holdsworth, R., Woodcock, N., & Strachan, R. (2000). Geological framework of Britain and Ireland. In N. Woodcock, & R. Strachan (Eds.), The Geological Framework of Britain and Ireland (19-37). Blackwell

Re-Os isotope characteristics of postorogenic lavas: Implications for the nature of young lithospheric mantle and its contribution to basaltic magmas (2000)
Journal Article
Schaefer, B., Turner, S., Rogers, N., Hawkesworth, C., Williams, H., Pearson, D., & Nowell, G. (2000). Re-Os isotope characteristics of postorogenic lavas: Implications for the nature of young lithospheric mantle and its contribution to basaltic magmas. Geology, 28(6), 563-566. https://doi.org/10.1130/0091-7613%282000%2928%3C563%3Aricopl%3E2.0.co%3B2

Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge-segments (2000)
Journal Article
Allerton, S., Escartin, J., & Searle, R. C. (2000). Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge-segments. Geology, 28, 179-182. https://doi.org/10.1130/0091-7613%282000%2928%3C179%3Aeamaoo%3E2.0.co%3B2

We report the results of a deep-towed magnetic survey of part of a Mid Atlantic Ridge spreading segment. Analysis of the magnetic reversals indicates that for the last 0.7 Ma, magmatic accretion at the end of the segment has been effectively one-side... Read More about Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge-segments.