Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject
Reinterpretation of old heat flow data or use of new data and new techniques of detection of the temperature under the surface have conducted to new heat flow density values in some regions of the globe. The problem of ice melting in Greenland and Antarctica caught the public's attention to the...
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ftunivevora:oai:dspace.uevora.pt:10174/18822 2023-09-05T13:15:04+02:00 Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject Duque, Maria Rosa Alves 2016-04 http://hdl.handle.net/10174/18822 por por EGU General Assembly Duque,M.R.(2016).Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject.EGU General Assembly 2016, Viena, Áustria, 18 a 22 de Abril de 2016. (C. Poster) http://hdl.handle.net/10174/18822 nao sim mrad@uevora.pt 393 restrictedAccess Fluxo de calor Condutividade térmica Gradiente de temperatura Litosfera Profundidade da Moho lecture 2016 ftunivevora 2023-08-14T17:39:57Z Reinterpretation of old heat flow data or use of new data and new techniques of detection of the temperature under the surface have conducted to new heat flow density values in some regions of the globe. The problem of ice melting in Greenland and Antarctica caught the public's attention to the importance of knowledge on heat flow values and thermal structure of the globe. In the last years, several models were presented trying to obtain lithosphere and Moho thickness of the Iberia Peninsula. The work we intend to present is related with the SW part of the Iberia Peninsula ( south of the Ossa Morena zone, South Portuguese Zone and Algarve). The results obtained show a decrease in the thickness of the crust and the lithosphere in this region. Density anomalies in the crust are also referred. I intend to make the connection between the results of these models and the heat flow thermal conductivity, heat production and geological data available for the region, trying to explain the results of heat flow density data obtained. Lecture Antarc* Antarctica Greenland Repositório Científico da Universidade de Évora Greenland Morena ENVELOPE(-67.121,-67.121,-68.580,-68.580) |
institution |
Open Polar |
collection |
Repositório Científico da Universidade de Évora |
op_collection_id |
ftunivevora |
language |
Portuguese |
topic |
Fluxo de calor Condutividade térmica Gradiente de temperatura Litosfera Profundidade da Moho |
spellingShingle |
Fluxo de calor Condutividade térmica Gradiente de temperatura Litosfera Profundidade da Moho Duque, Maria Rosa Alves Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject |
topic_facet |
Fluxo de calor Condutividade térmica Gradiente de temperatura Litosfera Profundidade da Moho |
description |
Reinterpretation of old heat flow data or use of new data and new techniques of detection of the temperature under the surface have conducted to new heat flow density values in some regions of the globe. The problem of ice melting in Greenland and Antarctica caught the public's attention to the importance of knowledge on heat flow values and thermal structure of the globe. In the last years, several models were presented trying to obtain lithosphere and Moho thickness of the Iberia Peninsula. The work we intend to present is related with the SW part of the Iberia Peninsula ( south of the Ossa Morena zone, South Portuguese Zone and Algarve). The results obtained show a decrease in the thickness of the crust and the lithosphere in this region. Density anomalies in the crust are also referred. I intend to make the connection between the results of these models and the heat flow thermal conductivity, heat production and geological data available for the region, trying to explain the results of heat flow density data obtained. |
format |
Lecture |
author |
Duque, Maria Rosa Alves |
author_facet |
Duque, Maria Rosa Alves |
author_sort |
Duque, Maria Rosa Alves |
title |
Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject |
title_short |
Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject |
title_full |
Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject |
title_fullStr |
Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject |
title_full_unstemmed |
Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject |
title_sort |
thermal models, lithosphere thickness and heat flow in south portugal. some comments about the subject |
publisher |
EGU General Assembly |
publishDate |
2016 |
url |
http://hdl.handle.net/10174/18822 |
long_lat |
ENVELOPE(-67.121,-67.121,-68.580,-68.580) |
geographic |
Greenland Morena |
geographic_facet |
Greenland Morena |
genre |
Antarc* Antarctica Greenland |
genre_facet |
Antarc* Antarctica Greenland |
op_relation |
Duque,M.R.(2016).Thermal models, lithosphere thickness and heat flow in South Portugal. Some comments about the subject.EGU General Assembly 2016, Viena, Áustria, 18 a 22 de Abril de 2016. (C. Poster) http://hdl.handle.net/10174/18822 nao sim mrad@uevora.pt 393 |
op_rights |
restrictedAccess |
_version_ |
1776196919204249600 |