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    by Lubomír NÁTR
    Published in Kvasny Prumysl (2006)
    ...Oceans cover some 3 quarters of the Earth's surface and play an important role in water and mineral...
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  3. 3
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    ... involving episodic ocean and ice-sheet formation. The formation of valley networks early in Mars' history...
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  5. 5
    ...Large temperature variations on land, in the air, and at the ocean surface, and highly variable...
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  6. 6
    ..., DOI 10.1016/j.crte.2006.05.012 Carton JA, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002817...
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  7. 7
    ..., DOI 10.1016/j.crte.2006.05.012 Carton JA, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002817...
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  8. 8
    ..., but it is also the origin of one of the most peculiar types of sea ice found in the polar oceans: platelet ice...
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  9. 9
  10. 10
    ... on sea level and ocean tides in Hudson Bay"...
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    Text
  11. 11
    ... and amorphous silica fluxes into the ocean during the last deglaciation, reaching values of ∼5.5 Tmol year−1...
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  12. 12
    ... and amorphous silica fluxes into the ocean during the last deglaciation, reaching values of ∼5.5 Tmol year−1...
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  13. 13
    ... and amorphous silica fluxes into the ocean during the last deglaciation, reaching values of ∼5.5 Tmol year(-1...
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  14. 14
    ..., DOI 10.1016/j.crte.2006.05.012 Carton JA, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002817...
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  15. 15
    ..., DOI 10.1016/j.crte.2006.05.012 Carton JA, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002817...
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  16. 16
    ..., DOI 10.1016/j.crte.2006.05.012 Carton JA, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002817...
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  17. 17
    ... and amorphous silica fluxes into the ocean during the last deglaciation, reaching values of ∼5.5 Tmol year -1...
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  18. 18
    ... and amorphous silica fluxes into the ocean during the last deglaciation, reaching values of ∼5.5 Tmol year -1...
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