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Volumn 188, Issue 1-2, 2011, Pages 9-25

Geothermal studies of the Outokumpu Deep Drill Hole, Finland: Vertical variation in heat flow and palaeoclimatic implications

Author keywords

Fennoscandian Shield; Geothermal gradient; Heat flow; Paleoclimatology; Thermal conductivity

Indexed keywords

CONDUCTIVE EFFECTS; CONDUCTIVE MODEL; CONVECTION CELL; DATA SETS; DRILL HOLE; EASTERN FINLAND; FENNOSCANDIAN SHIELDS; FINLAND; FLUID FLOW EFFECT; GEOTHERMAL GRADIENTS; GROUND SURFACE TEMPERATURE; HEAT FLOW DENSITY; HEAT FLOWS; HEAT TRANSFER PROCESS; HIGH RESOLUTION; HOLOCENES; HYDRAULIC HEADS; INVERSE TRANSIENT; LARGE DIAMETER; METASEDIMENTARY ROCKS; PALEOCLIMATOLOGY; SALINE FORMATION; SURFACE HEAT FLOW; TEMPERATURE GRADIENT; TEMPERATURE VARIATION; THERMAL CONDUCTIVITY MEASUREMENTS; THERMAL CONVECTIONS; THERMAL DISTURBANCE; ULTRAMAFIC ROCKS; VERTICAL VARIATION;

EID: 80053316188     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2011.06.002     Document Type: Article
Times cited : (47)

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