Science: v.1-v.219Moses King, 1969 |
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Стр. 996
... determined by analyses of their volcanic features . Top : left , pillow D19 ( 61 by 48 by 30 cm ) ; right , two views of the crust D38 ( 38 by 30 by 8 cm ) . Bottom : two views of pillow D17 ( 30 by 30 by 23 cm ) . ever , lack of ...
... determined by analyses of their volcanic features . Top : left , pillow D19 ( 61 by 48 by 30 cm ) ; right , two views of the crust D38 ( 38 by 30 by 8 cm ) . Bottom : two views of pillow D17 ( 30 by 30 by 23 cm ) . ever , lack of ...
Стр. 1269
... determined by simple examination of the profiles which anomaly is present . In order to overcome this difficulty the age of each pertinent anomaly was determined for all the profiles from the assumed con- stant spreading rates from 3.32 ...
... determined by simple examination of the profiles which anomaly is present . In order to overcome this difficulty the age of each pertinent anomaly was determined for all the profiles from the assumed con- stant spreading rates from 3.32 ...
Стр. 1277
... determined by sedimentation equilibrium ( 7 ) . Both carboxylases were maintained in the protomeric form for molecular weight and sedimentation velocity ( analytical ultracentrifuge ) determination with 0.5M NaCl and 50 mM tris ...
... determined by sedimentation equilibrium ( 7 ) . Both carboxylases were maintained in the protomeric form for molecular weight and sedimentation velocity ( analytical ultracentrifuge ) determination with 0.5M NaCl and 50 mM tris ...
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