A Fine-Scale Seismic Stratigraphy of the Eastern Margin of the Weddell Sea

Author(s):  
H. Miller ◽  
J. P. Henriet ◽  
N. Kaul ◽  
A. Moons
Geology ◽  
1978 ◽  
Vol 6 (10) ◽  
pp. 635 ◽  
Author(s):  
Thomas H. Shipley ◽  
Joel S. Watkins

2004 ◽  
Vol 25 (3-4) ◽  
pp. 265-282 ◽  
Author(s):  
J. Rogenhagen ◽  
W. Jokat ◽  
K. Hinz ◽  
Y. Kristoffersen

Antarctica ◽  
2006 ◽  
pp. 441-446 ◽  
Author(s):  
Andrés Maldonado ◽  
Antonio Barnolas ◽  
Fernando Bohoyo ◽  
Carlota Escutia ◽  
Jesús Galindo-ZaldÍvar ◽  
...  

Author(s):  
Russell L. Steere

Complementary replicas have revealed the fact that the two common faces observed in electron micrographs of freeze-fracture and freeze-etch specimens are complementary to each other and are thus the new faces of a split membrane rather than the original inner and outer surfaces (1, 2 and personal observations). The big question raised by published electron micrographs is why do we not see depressions in the complementary face opposite membrane-associated particles? Reports have appeared indicating that some depressions do appear but complementarity on such a fine scale has yet to be shown.Dog cardiac muscle was perfused with glutaraldehyde, washed in distilled water, then transferred to 30% glycerol (material furnished by Dr. Joaquim Sommer, Duke Univ., and VA Hospital, Durham, N.C.). Small strips were freeze-fractured in a Denton Vacuum DFE-2 Freeze-Etch Unit with complementary replica tooling. Replicas were cleaned in chromic acid cleaning solution, then washed in 4 changes of distilled water and mounted on opposite sides of the center wire of a Formvar-coated grid.


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