Publicação

Can heat flow be related with pyrite contente and location in the Iberian Pyrite Belt (Portugal)?

Detalhes bibliográficos
Resumo:	The heat flow density and temperature data obtained in part of the South Portuguese Zone in Portugal are analyzed in this work. Part of the Iberian Pyrite Belt is located in the region studied. The heat flow values are higher than average values found in continental regions and the excess of heat found can not be provided by radioactivity sources in the region like uranium, thorium and potassium. The excess of heat is obtained considering that the anomalous sources of heat are located in a uniform layer with a thickness of 6 Km. The difference between the average value of heat sources and the radioactivity sources (D-A) is directly related with the heat flow values measured in the region. High thermal gradient values can be found in neighboring regions with low thermal conductivity values suggesting the existence of lateral heat transfer. It is suggested that the excess of heat is due to chemical reactions involving oxidation of pyrite ores abundant in the region. At the end a question is made. Why not use the heat flow in the detection of pyrite bodies in the region ?
Autores principais:	Duque, Maria Rosa
Assunto:	heat flow anomaly heat sources thermal gradients thermal conductivity Iberian Pyrite belt
Ano:	2019
País:	Portugal
Tipo de documento:	artigo
Tipo de acesso:	acesso restrito
Instituição associada:	Universidade de Évora
Idioma:	inglês
Origem:	Repositório Científico da Universidade de Évora

Descrição
Resumo:	The heat flow density and temperature data obtained in part of the South Portuguese Zone in Portugal are analyzed in this work. Part of the Iberian Pyrite Belt is located in the region studied. The heat flow values are higher than average values found in continental regions and the excess of heat found can not be provided by radioactivity sources in the region like uranium, thorium and potassium. The excess of heat is obtained considering that the anomalous sources of heat are located in a uniform layer with a thickness of 6 Km. The difference between the average value of heat sources and the radioactivity sources (D-A) is directly related with the heat flow values measured in the region. High thermal gradient values can be found in neighboring regions with low thermal conductivity values suggesting the existence of lateral heat transfer. It is suggested that the excess of heat is due to chemical reactions involving oxidation of pyrite ores abundant in the region. At the end a question is made. Why not use the heat flow in the detection of pyrite bodies in the region ?