Use of chemical geothermometry and heat loss models in estimating terrestrial heat flow for low-temperature hydrothermal systems (1988)
- Autor:
- Autor USP: HURTER, SUZANNE JACQUELINE - IAG
- Unidade: IAG
- Assunto: GEOFÍSICA
- Language: Português
- Imprenta:
- Source:
- Título: Revista Brasileira de Geofisica
- Volume/Número/Paginação/Ano: v.6 , n.2 , p.33-42, jun./dez. 1988
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ABNT
HURTER, S J. Use of chemical geothermometry and heat loss models in estimating terrestrial heat flow for low-temperature hydrothermal systems. Revista Brasileira de Geofisica, v. 6 , n. ju/dez. 1988, p. 33-42, 1988Tradução . . Acesso em: 05 mar. 2026. -
APA
Hurter, S. J. (1988). Use of chemical geothermometry and heat loss models in estimating terrestrial heat flow for low-temperature hydrothermal systems. Revista Brasileira de Geofisica, 6 ( ju/dez. 1988), 33-42. -
NLM
Hurter SJ. Use of chemical geothermometry and heat loss models in estimating terrestrial heat flow for low-temperature hydrothermal systems. Revista Brasileira de Geofisica. 1988 ;6 ( ju/dez. 1988): 33-42.[citado 2026 mar. 05 ] -
Vancouver
Hurter SJ. Use of chemical geothermometry and heat loss models in estimating terrestrial heat flow for low-temperature hydrothermal systems. Revista Brasileira de Geofisica. 1988 ;6 ( ju/dez. 1988): 33-42.[citado 2026 mar. 05 ] - Thermal structure of the parana basin , southern brazil
- Heat flow from the earth's interior: analysis of the global data set
- Thermal structure of the parana basin (brazil) from inversion of bottom-hole temperature data
- Cooling of igneous rocks from the serra geral event
- Effect of the cretaceous serra geral igneous event on the temperatures and heat flow of the parana basin , southern brazil
- Geothermal effects in sediments of the parana basin in southern brazil as recorded by illite crystallinity
- New global heat flow data base
- Effects of basin scale fluid flow on the heat flow of the parana basin, southern brazil
- Transport of geothermal heat by inter-fracture fluid flows
- Aplicação de geotermometros químicos em águas de fontes brasileiras na determinação do fluxo geotérmico
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