Articles Alert

GEOSCIENCES BY PETER J. SMITH Department of Earth Sciences Open University Milton Keynes, U.K. " Seismic reflection studies in the North Atlantic, southwest of Bermuda, show that the oceanic crust is not as uniform as hitherto supposed. In particular, dipping reflectors in the lower crust indicate either major fault zones or, more probably, chemical signatures of magma chambers once active on the mid-Atlantic ridge, note the authors of a new study. J. McCarthy, J.C. Mutter, J.L. Morton, N.H.

Written byPeter Smith

| 2 min read

Save for Later

Listen with Speechify

0:00

2:00

BY PETER J. SMITH
Department of Earth Sciences
Open University
Milton Keynes, U.K.

" Seismic reflection studies in the North Atlantic, southwest of Bermuda, show that the oceanic crust is not as uniform as hitherto supposed. In particular, dipping reflectors in the lower crust indicate either major fault zones or, more probably, chemical signatures of magma chambers once active on the mid-Atlantic ridge, note the authors of a new study.

J. McCarthy, J.C. Mutter, J.L. Morton, N.H. Sleep, G.A. Thompson, “Relic magma chamber structures preserved within the Mesozoic North Atlantic crust?,” Geological Society of America Bulletin, 100 (9), 1423-36, September 1988.

" The characteristics of the Caledonian orogenic belts, ophiolotes, sediments, and faunal provinces in Britain and Scandinavia indicate ocean-margin terrane processes rather than the opening and closing of a major ocean. The supposed lapetus, or Proto-Atlantic, Ocean may never have existed.

R. Mason, “Did the Iapetus Ocean really exist?,” ...

Interested in reading more?

Become a Member of

Receive full access to digital editions of The Scientist, as well as TS Digest, feature stories, more than 35 years of archives, and much more!

Join for free today

Already a member? Login Here