Nature, Volume 253 |
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Page 323
It is suggested that the spreading activity in the Labrador Sea during phase I was
coupled to spreading in the Bay of Biscay”. About 60 Myr ago the East and West
Thulean Rises were one ridge system, as can be demonstrated by reversing the
...
It is suggested that the spreading activity in the Labrador Sea during phase I was
coupled to spreading in the Bay of Biscay”. About 60 Myr ago the East and West
Thulean Rises were one ridge system, as can be demonstrated by reversing the
...
Page 337
... incidence terms, we obtain the synthetic seismograms. In our present
computation we used M = 5.0 × 10” dyne cm, the value suggested by Dziewonski
and Gilbert", o = 8.5 km s−" and p = 3.5 g cm To for the average upper d Time (
min) Fig.
... incidence terms, we obtain the synthetic seismograms. In our present
computation we used M = 5.0 × 10” dyne cm, the value suggested by Dziewonski
and Gilbert", o = 8.5 km s−" and p = 3.5 g cm To for the average upper d Time (
min) Fig.
Page 506
But the boundaries of these divisions have yet to be decided, and may not
correspond to the values suggested here, in which case this scheme might be
modified accordingly. Precambrian divisions along these lines have been
proposed”.
But the boundaries of these divisions have yet to be decided, and may not
correspond to the values suggested here, in which case this scheme might be
modified accordingly. Precambrian divisions along these lines have been
proposed”.
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