Nature, Volume 253 |
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Page 172
We can see from equation (2) that as an ice stream is slowed down as it moves
out into a uniform ice shelf, the change of stress in the direction of flow, and
hence by simple theory of the ice thickness, must be balanced by a gradient of
shear ...
We can see from equation (2) that as an ice stream is slowed down as it moves
out into a uniform ice shelf, the change of stress in the direction of flow, and
hence by simple theory of the ice thickness, must be balanced by a gradient of
shear ...
Page 501
Finally, since the predominant chilled margin direction is the direction away from
the spreading centre, it follows from the data above that the spreading axis
should have lain relatively to the west of the Troodos complex. It is necessary to
say ...
Finally, since the predominant chilled margin direction is the direction away from
the spreading centre, it follows from the data above that the spreading axis
should have lain relatively to the west of the Troodos complex. It is necessary to
say ...
Page 519
The average standard deviation in the direction perpendicular to the plane,
based on the estimate of 0.39 for G, is 3.5 km. Thus, We have good accuracy
perpendicular to the zone below about 120 km but not above that depth, where
the zone ...
The average standard deviation in the direction perpendicular to the plane,
based on the estimate of 0.39 for G, is 3.5 km. Thus, We have good accuracy
perpendicular to the zone below about 120 km but not above that depth, where
the zone ...
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Bibliographic information
| Title | Nature, Volume 253 Marilee E. Thomas and Robert C. Thomas Science and Related Subjects Collection |
| Editor | Sir Norman Lockyer |
| Publisher | Macmillan Journals Limited, 1975 |
| Original from | the University of Michigan |
| Digitized | 16 Jul 2009 |
| Export Citation | BiBTeX EndNote RefMan |