Page
%P
![Loading...](https://link.springer.com/static/c4a417b97a76cc2980e3c25e2271af3129e08bbe/images/pdf-preview/spacer.gif)
-
Article
Inorganic-organic interactions: implications for gas isotope interpretation
-
Chapter
Flow Along Fractures in Sedimentary Basins
Sedimentary basins are large depressions in the earth’s crust containing from a few to more than 15 km of sediments. At deposition, sediments may contain in excess of 50% water; huge volumes of fluids are thus...