Pregled bibliografske jedinice broj: 148784
Prilog poznavanju gustoće površinskog toplinskog toka u širem području Zagreba
Prilog poznavanju gustoće površinskog toplinskog toka u širem području Zagreba // Procidings of the First Croatian Geological Congress / Vlahović, Igor ; Velić, Ivo ; Šparica, Marko (ur.).
Zagreb: Hrvatski geološki institut, 1995. str. 303-306 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), ostalo)
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Naslov
Prilog poznavanju gustoće površinskog toplinskog toka u širem području Zagreba
(COTRIBUTION TO KNOWLEDGE ON TERRESTRIAL HEAT-FLOW DENSITY IN THE GREATER AREA OF ZAGREB)
Autori
Kovačić, Miron
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), ostalo
Izvornik
Procidings of the First Croatian Geological Congress
/ Vlahović, Igor ; Velić, Ivo ; Šparica, Marko - Zagreb : Hrvatski geološki institut, 1995, 303-306
Skup
1. Hrvatski Geološki kongres = The First Croatian Geological Congress
Mjesto i datum
Opatija, Hrvatska, 18.10.1995. - 21.10.1995
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
geotermija; gustoća toplinskog toka; geotermijska anomalija; Zagreb
(geothermic; heat-flow density; geothermal anomaly Zagreb)
Sažetak
Within the project Basic Geothermic Map of the Republic of Croatia investigation on terrestrial heat-flow density in the greater area of Zagreb was carried out. The calculation was based on temperature data for deep drill-holes and conductivity of the drilled lithologic units. It has been determined that values of geothermic gradients, rock thermal conductivities, interval heat-flow densities and terrestrial heat-flow densities are of wide range. Terrestrial heat-flow density values in the narrow zone of the investigated area are considerably higher than the average and are typical of positive anomalies of terrestrial heat-flow density. Positive anomaly of terrestrial heat-flow density is somewhat wider than positive temperature anomaly at the depth of 1000 m. Values of terrestrial heat-flow density obtained by this investigation differ from data published so far.
Izvorni jezik
Hrvatski
Znanstvena područja
Geologija
POVEZANOST RADA