The concentrations of copper (~ 10~8M), however, were far in excess of their theoretical values had they been controlled by ... The changes in copper were obtained by integration between the sill depth and the basin floor over the time period between observations. ... The results of that exercise are listed in table 18- 2.
|Title||:||The Dynamic environment of the ocean floor|
|Author||:||Kent A. Fanning, Frank T. Manheim|
|Publisher||:||Free Press - 1981-10|