35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341

A 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...

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Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
North Atlantic
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9451
http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.584.9451 2023-05-15T17:30:59+02:00 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9451 http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9451 http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf text ftciteseerx 2016-01-08T13:12:45Z A 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. Text North Atlantic Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description A 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.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341
spellingShingle 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341
title_short 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341
title_full 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341
title_fullStr 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341
title_full_unstemmed 35. AN ESTIMATE OF THE HEAT FLOW IN THE WESTERN NORTH ATLANTIC AT DEEP SEA DRILLING PROJECT SITE 5341
title_sort 35. an estimate of the heat flow in the western north atlantic at deep sea drilling project site 5341
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9451
http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf
genre North Atlantic
genre_facet North Atlantic
op_source http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9451
http://www.deepseadrilling.org/76/volume/dsdp76_35.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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