Sr-Nd-Pb isotopes of Tertiary volcanics of King George Island, Antarctica

1997 ◽  
Vol 42 (22) ◽  
pp. 1913-1918 ◽  
Author(s):  
Guangfu Xing ◽  
Weizhou Shen ◽  
Dezi Wang ◽  
Qingmin Jin
Keyword(s):  
Pb Isotopes ◽  
King George Island

Antarctic harpacticoids exploit different trophic niches: a summer snapshot using fatty acid trophic markers (Potter Cove, King George Island)

2017 ◽  
Vol 568 ◽  
pp. 59-71
Author(s):  
E Werbrouck ◽  
A Vanreusel ◽  
D Deregibus ◽  
D Van Gansbeke ◽  
M De Troch
Keyword(s):  
Fatty Acid ◽  
King George Island ◽  
Potter Cove ◽  
Trophic Markers ◽  
Trophic Niches

205Bi/206Bi cyclotron production from Pb-isotopes for absorption studies in humans

1993 ◽  
Vol 44 (12) ◽  
pp. 1467-1472
Author(s):  
R. Fischer ◽  
J. Wendel ◽  
B. Dresow ◽  
V. Bechtold ◽  
H.C. Heinrich
Keyword(s):  
Pb Isotopes ◽  
Cyclotron Production ◽  
Absorption Studies

Trophic niche of seabirds on the Barton Peninsula, King George Island, Antarctica

2021 ◽  
pp. 107443
Author(s):  
Jong-Ku Gal ◽  
Bohyung Choi ◽  
Bo-Kyung Kim ◽  
Jin-Woo Jung ◽  
Jun-Oh Min ◽  
...  
Keyword(s):  
Trophic Niche ◽  
King George Island ◽  
Barton Peninsula

Genesis and Hydrothermal Evolution of the Zhazigou Skarn W (Mo) Deposit, East Qinling, China: Constraints from Fluid Inclusions and H–O–S–Pb isotopes

2021 ◽  
pp. 104374
Author(s):  
Liwei Xue ◽  
Gongwen Wang ◽  
Li Tang ◽  
Yi Cao ◽  
Jingguo Du ◽  
...  
Keyword(s):  
Fluid Inclusions ◽  
Pb Isotopes

scholarly journals Glacier Geometry Changes in the Western Shore of Admiralty Bay, King George Island over the Last Decades

Sensors ◽  
2021 ◽  
Vol 21 (4) ◽  
pp. 1532
Author(s):  
Mariusz Pasik ◽  
Krzysztof Bakuła ◽  
Sebastian Różycki ◽  
Wojciech Ostrowski ◽  
Maria Elżbieta Kowalska ◽  
...  
Keyword(s):  
Protected Area ◽  
Average Rate ◽  
King George Island ◽  
Glacier Surface ◽  
Glacial Retreat ◽  
Glacier Front ◽  
Longitudinal Slope ◽  
Western Shore ◽  
Rapid Temperature

This paper presents changes in the range and thickness of glaciers in Antarctic Specially Protected Area (ASPA) No. 128 on King George Island in the period 1956–2015. The research indicates an intensification of the glacial retreat process over the last two decades, with the rate depending on the type of glacier front. In the period 2001–2015, the average recession rate of the ice cliffs of the Ecology Glacier and the northern part of the Baranowski Glacier was estimated to be approximately 15–25 m a−1 and 10–20 m a−1, respectively. Fronts of Sphinx Glacier and the southern part of the Baranowski Glacier, characterized by a gentle descent onto land, show a significantly lower rate of retreat (up to 5–10 m a−1 1). From 2001 to 2013, the glacier thickness in these areas decreased at an average rate of 1.7–2.5 m a−1 for the Ecology Glacier and the northern part of the Baranowski Glacier and 0.8–2.5 m a−1 for the southern part of the Baranowski Glacier and Sphinx Glacier. The presented deglaciation processes are related to changes of mass balance caused by the rapid temperature increase (1.0 °C since 1948). The work also contains considerations related to the important role of the longitudinal slope of the glacier surface in the connection of the glacier thickness changes and the front recession.

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