| 000 | 01212nam a22002777a 4500 | ||
|---|---|---|---|
| 001 | GENERAL-000881 | ||
| 003 | EC-OLADE-CDD | ||
| 005 | 20160922142207.0 | ||
| 008 | 160705b xxu||||| |||| 00| 0 spa d | ||
| 040 |
_aOLADE-CDD _cOLADE-CDD |
||
| 041 | _aeng | ||
| 082 |
_a333.88 _bA8466 / 1978 |
||
| 100 | _aSmith, R. L. | ||
| 700 | _aShaw, H. R. | ||
| 245 | _aIgneous - related geothermal systems. En : Assessment of geothermal resources of the United States | ||
| 260 |
_aArlington _bUnited States Department of Interior _c1979 |
||
| 300 | _app. 12-18 | ||
| 504 | _a07424 | ||
| 500 | _aImpreso | ||
| 520 | _aCalculations based on conductive cooling of magma indicate that 101,000 x 10(18) H still remains in evaluated young ingenous - related systems of the United States to a depth of 10 km. The total energy in both evaluated and unevaluated young igneous - related systems is estimated to be an order of magnitude greater. Recent studies of the effects of hydrothermal processes on the cooling of a pluton do not change the conclusions of Smith and Shaw... | ||
| 650 | _aGEOTERMIA | ||
| 650 | _aRECURSOS GEOTERMICOS | ||
| 650 | _aCONGRESOS Y CONFERENCIAS | ||
| 651 | _aUSA | ||
| 942 |
_2ddc _cBK |
||
| 999 |
_c5784 _d5784 |
||