scholarly journals Lithostratigraphy determined from downhole logs in the AND-2A borehole, southern Victoria Land Basin, McMurdo Sound, Antarctica

Geosphere ◽  
2012 ◽  
Vol 9 (1) ◽  
pp. 63-73 ◽  
Author(s):  
S. Hunze ◽  
H. Schroder ◽  
G. Kuhn ◽  
T. Wonik
Keyword(s):  
Mcmurdo Sound ◽  
Victoria Land ◽  
Victoria Land Basin

Environmental magnetic record of Antarctic palaeoclimate from Eocene/Oligocene glaciomarine sediments, Victoria Land Basin

1998 ◽  
Vol 134 (3) ◽  
pp. 653-662 ◽  
Author(s):  
Leonardo Sagnotti ◽  
Fabio Florindo ◽  
Kenneth L. Verosub ◽  
Gary S. Wilson ◽  
Andrew P. Roberts
Keyword(s):  
Victoria Land ◽  
Magnetic Record ◽  
Victoria Land Basin ◽  
Glaciomarine Sediments

scholarly journals Large Salt Beds on the Surface of the Ross Ice Shelf Near Black Island, Antarctica

1981 ◽  
Vol 27 (95) ◽  
pp. 11-18 ◽  
Author(s):  
Howard Thomas Brady ◽  
Barry Batts
Keyword(s):  
Thin Layer ◽  
Dry Valleys ◽  
Ice Shelf ◽  
Mcmurdo Sound ◽  
Extensive System ◽  
Ross Ice Shelf ◽  
Victoria Land ◽  
Marine Algal ◽  
Algal Mat

AbstractAn extensive system of mirabilite (Na2SO4· 10H2O) beds has been mapped on the Ross Ice Shelf near Black Island. The salt beds are normally underlain by a thin layer of mud and their surface is covered by a non-marine algal mat and boulder lag. These authors suggest the salt has been formed by the displacement of sub-ice-shelf brines to the ice-shelf surface. Evidence also suggests that other terrestrial mirabilite beds in the McMurdo Sound area were formed in the same manner and deposited by the Ross Ice Shelf during its Wisconsin retreat from McMurdo Sound. Mirabilite salt in the dry valleys, southern Victoria Land, may have also originated from melt waters which dissolved ice-shelf mirabilite beds.

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