Within the same context the release of juvenile water tied up in fossil fuels like coal, lignite, gas and petrol is generally overlooked.
2.
The ?D values of hydroxyl-bearing minerals of mantle were estimated to be-800 ~-400 through the analysis of the isotopic composition for juvenile water.
3.
They are cold-blooded animals that metamorphose from a juvenile water-breathing form, usually to an adult air-breathing form, though mudpuppies retain juvenile gills in adulthood.
4.
The H isotope composition of mantle water is around-800 ~-500 depending on its states such as fluid, hydrous phase, hydroxyl point defect, Juvenile water ( from degassing of the mantle ), magmatic water ( water equilibrated with a magma ).
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