Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands
Information on temperature, temperature gradients, thermal conductivity and heat flow from the c. 3.5 km deep Lopra-1/1A borehole in the Faroe Islands is presented and analysed. The upper 2450 m of the drilled sequence consists of thick tholeiitic basalt flows and the deeper parts of hyaloclastites...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.535.7052 2023-05-15T16:10:39+02:00 Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands Niels Balling Niels Breiner Regin Waagstein The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.7052 http://www.geus.dk/publications/bull/nr9/nr9_p91-107.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.7052 http://www.geus.dk/publications/bull/nr9/nr9_p91-107.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geus.dk/publications/bull/nr9/nr9_p91-107.pdf text ftciteseerx 2016-01-08T10:48:27Z Information on temperature, temperature gradients, thermal conductivity and heat flow from the c. 3.5 km deep Lopra-1/1A borehole in the Faroe Islands is presented and analysed. The upper 2450 m of the drilled sequence consists of thick tholeiitic basalt flows and the deeper parts of hyaloclastites and thin beds of basalt. Temperature data originate from high precision temperature logging a long time after drilling to a depth of 2175 m (the original Lopra-1 borehole) and from commercial tempe-rature logs measured a short time after drilling to a depth of 3430 m (Lopra-1/1A). The high-preci-sion temperature log determines accurately levels of inflow of groundwater to the borehole and signif-icant thermal disturbances to a depth of c. 1250 m. Below 1300 m, no significant disturbances are seen and interval temperature gradients for large depth intervals show only small variations between 28 and 33°C/km. The mean least-squares gradient for the depth interval of 1400–3430 m is 31.4°C/ km. In clear contrast to these overall very homogeneous, large-interval, mean temperature gradients, great local variability, between gradients of 20–25°C/km and 45°C/km, was observed between about 1300 and 2175 m (maximum depth of the high-resolution temperature log). These gradient varia-tions are interpreted to be due to thermal conductivity variations and to reflect varying secondary mineralisation and mineral alterations. Text Faroe Islands Unknown Faroe Islands Lopra ENVELOPE(-6.771,-6.771,61.444,61.444) Sion ENVELOPE(13.758,13.758,66.844,66.844) |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
Information on temperature, temperature gradients, thermal conductivity and heat flow from the c. 3.5 km deep Lopra-1/1A borehole in the Faroe Islands is presented and analysed. The upper 2450 m of the drilled sequence consists of thick tholeiitic basalt flows and the deeper parts of hyaloclastites and thin beds of basalt. Temperature data originate from high precision temperature logging a long time after drilling to a depth of 2175 m (the original Lopra-1 borehole) and from commercial tempe-rature logs measured a short time after drilling to a depth of 3430 m (Lopra-1/1A). The high-preci-sion temperature log determines accurately levels of inflow of groundwater to the borehole and signif-icant thermal disturbances to a depth of c. 1250 m. Below 1300 m, no significant disturbances are seen and interval temperature gradients for large depth intervals show only small variations between 28 and 33°C/km. The mean least-squares gradient for the depth interval of 1400–3430 m is 31.4°C/ km. In clear contrast to these overall very homogeneous, large-interval, mean temperature gradients, great local variability, between gradients of 20–25°C/km and 45°C/km, was observed between about 1300 and 2175 m (maximum depth of the high-resolution temperature log). These gradient varia-tions are interpreted to be due to thermal conductivity variations and to reflect varying secondary mineralisation and mineral alterations. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Niels Balling Niels Breiner Regin Waagstein |
spellingShingle |
Niels Balling Niels Breiner Regin Waagstein Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands |
author_facet |
Niels Balling Niels Breiner Regin Waagstein |
author_sort |
Niels Balling |
title |
Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands |
title_short |
Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands |
title_full |
Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands |
title_fullStr |
Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands |
title_full_unstemmed |
Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands |
title_sort |
thermal structure of the deep lopra-1/1a borehole in the faroe islands |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.7052 http://www.geus.dk/publications/bull/nr9/nr9_p91-107.pdf |
long_lat |
ENVELOPE(-6.771,-6.771,61.444,61.444) ENVELOPE(13.758,13.758,66.844,66.844) |
geographic |
Faroe Islands Lopra Sion |
geographic_facet |
Faroe Islands Lopra Sion |
genre |
Faroe Islands |
genre_facet |
Faroe Islands |
op_source |
http://www.geus.dk/publications/bull/nr9/nr9_p91-107.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.7052 http://www.geus.dk/publications/bull/nr9/nr9_p91-107.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1765995815231291392 |