Add to ORKGA method employing both a simple relationship between total rock conductivity and the concentrations and conduc-tivities of constituents, and an estimate of the thermal gradient based on a downhole temperature log, yielded an estimated value between 1.01 (42 mW m~2) and 1.37 HFU (57 mW m~2) for the heat flow at Site 534. These measure-ments are in good agreement with other heat-flow measurements made in the same area, indicating that this method may have a wide application in estimating heat flow at well sites
The subject of this article is the measurement of thermal flow under laboratory conditions. We can d...
At Hole 511, on the margin of Maurice Ewing Bank, eastern Falkland Plateau, successful bottom hole t...
Determination of the rate and distribution of heat flow through the Earth's crust provides one ...
Heat-flow measurements have been made in two holes at Deep Sea Drilling Project Site 465, southern H...
Measurements of temperature gradients in sediments, thermal conductivity and drill-hole temperatures...
Successful downhole temperature measurements were made at Sites 225, 227, and 228, enabling reasonab...
Downhole temperatures and sediment thermal conductivities measured on Leg 65 of the Deep Sea Drillin...
Heat flow estimates at two sites on the U.S. Atlantic continental margin are presented. An estimate...
An apparatus to measure heat flow through the ocean floor in con-junction with standard coring techn...
The geothermal heat flow measured at the surface of the Earth is originated by different heat sourc...
Using a new temperature recording instrument recently developed at the Woods Hole Oceanographic Inst...
This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey edit...
Thirty-four sediment and mud line temperatures were collected from six drill holes on Ocean Drilling...
Thirty-four sediment and mudline temperatures were collected from six drill holes on ODP Leg 110 nea...
During cruises in the Norwegian Sea in 1969 and 1972 seven heat flow values were measured between Ic...
The subject of this article is the measurement of thermal flow under laboratory conditions. We can d...
At Hole 511, on the margin of Maurice Ewing Bank, eastern Falkland Plateau, successful bottom hole t...
Determination of the rate and distribution of heat flow through the Earth's crust provides one ...
Heat-flow measurements have been made in two holes at Deep Sea Drilling Project Site 465, southern H...
Measurements of temperature gradients in sediments, thermal conductivity and drill-hole temperatures...
Successful downhole temperature measurements were made at Sites 225, 227, and 228, enabling reasonab...
Downhole temperatures and sediment thermal conductivities measured on Leg 65 of the Deep Sea Drillin...
Heat flow estimates at two sites on the U.S. Atlantic continental margin are presented. An estimate...
An apparatus to measure heat flow through the ocean floor in con-junction with standard coring techn...
The geothermal heat flow measured at the surface of the Earth is originated by different heat sourc...
Using a new temperature recording instrument recently developed at the Woods Hole Oceanographic Inst...
This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey edit...
Thirty-four sediment and mud line temperatures were collected from six drill holes on Ocean Drilling...
Thirty-four sediment and mudline temperatures were collected from six drill holes on ODP Leg 110 nea...
During cruises in the Norwegian Sea in 1969 and 1972 seven heat flow values were measured between Ic...
The subject of this article is the measurement of thermal flow under laboratory conditions. We can d...
At Hole 511, on the margin of Maurice Ewing Bank, eastern Falkland Plateau, successful bottom hole t...
Determination of the rate and distribution of heat flow through the Earth's crust provides one ...