Browsing PANGAEA by Title
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Browsing PANGAEA by Title
Now showing items 1566-1585 of 1650
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(PANGAEA, 2003-08-25)
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(PANGAEA, 2009-09-27)The sediment temperature distribution at mud volcanoes provides insights into their activity and into the occurrence of gas hydrates. If ambient pressure and temperature conditions are close to the limits of the gas hydrate ...
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(PANGAEA, 2000-09-25)
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(PANGAEA, 2001-07-18)
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(PANGAEA, 2002-05-05)Oil polluted and not oil polluted soils (crude oil hydrocarbons contents: 20-92500 mg/kg dry soil mass) under natural grass and forest vegetation and in a bog in the Russian tundra were compared in their principal soil ...
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(PANGAEA, 1988-03-15)
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(PANGAEA, 1984-03-19)
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(PANGAEA, 2010-09-13)The results of the International Permafrost Association's International Polar Year Thermal State of Permafrost (TSP) project are presented based on field measurements from Russia during the IPY years (2007-09) and collected ...
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(PANGAEA, 1997-04-05)
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(PANGAEA, 2003-03-20)
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(PANGAEA, 2009-10-19)Structural-petrologic and isotopic-geochronologic data on magmatic, metamorphic, and metasomatic rocks from the Chernorud zone were used to reproduce the multistage history of their exhumation to upper crustal levels. The ...
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Thermokarst in Siberian ice-rich permafrost: Comparison to asymmetric scalloped depressions on Mars. (PANGAEA, 2011-04-18)This data set provides a high-resolution digital elevation model (DEM) of a thermokarst depression (~7 km²) on ice-complex deposits in the Arctic Lena Delta, Siberia. The DEM based on a geodetic field survey and was used ...
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(PANGAEA, 2013-05-02)
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(PANGAEA, 2000-11-20)
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(PANGAEA, 2018-06-18)Most of the world's permafrost is located in the Arctic, where its frozen organic carbon con-tent makes it a potentially important influence on the global climate system. The Arctic climate appears to be changing more ...
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(PANGAEA, 2008-07-10)
Now showing items 1566-1585 of 1650