摘要：Due to the geothermal gradient or magmatic activities in deeply buried stratum, dry hot rock, high temperature and high-pressure brine bearing layers, or other high temperature reservoirs are commonly developed under gas hydrate reservoirs (Yamano M et al., 1986). As a result, a set of equipment based on a thermoelectric generator could use the natural high temperature fluids or dry hot rocks as heat sources for gas hydrate exploitation.
