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Polyak, Boris G; Fernàndez, Manel; Khutorskoy, Mikhail D; Soto, J I; Basov, Ivan A; Comas, Maria C; Khain, V Ye; Alonso, B; Agapova, Galina V; Mazurova, I S; Negredo, A; Tochitsky, V O; de La Linde Rubio, Joaquin; Bogdanov, Nikita A; Banda, E (1996): Component parts of the World Heat Flow Data Collection. PANGAEA, https://doi.org/10.1594/PANGAEA.805526

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Related to:
International Heat Flow Commission, I H F C (2012): Global Heat Flow Database. The Global Heat Flow Database of the International Heat Flow Commission (IHFC), University of North Dakota, USA; (data copied, 2012-10), http://www.heatflow.und.edu/index2.html
Polyak, Boris G; Fernàndez, Manel; Khutorskoy, Mikhail D; Soto, J I; Basov, Ivan A; Comas, Maria C; Khain, V Ye; Alonso, B; Agapova, Galina V; Mazurova, I S; Negredo, A; Tochitsky, V O; de La Linde Rubio, Joaquin; Bogdanov, Nikita A; Banda, E (1996): Heat flow in the Alboran Sea, western Mediterranean. Tectonophysics, 263, 191-218, https://doi.org/10.1016/0040-1951(95)00178-6
Further details:
Jessop, Alan M; Hobart, Michael A; Sclater, John G (1976): The World Heat Flow Data Collection - 1975. Geological Survey of Canada, Earth Physics Branch, Geothermal Series, 5, 10 pp, hdl:10013/epic.40176.d002
Coverage:
Median Latitude: 36.072827 * Median Longitude: -3.618449 * South-bound Latitude: 35.550000 * West-bound Longitude: -5.006700 * North-bound Latitude: 36.525000 * East-bound Longitude: -1.100000
Minimum ELEVATION: -2530 m a.s.l. * Maximum ELEVATION: -116 m a.s.l.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Area/localityAreaPolyak, Boris G
2Sample, optional label/labor noLab noPolyak, Boris G
3LATITUDELatitudeGeocode
4LONGITUDELongitudeGeocode
5ELEVATIONElevationm a.s.l.Geocode
6Depth, top/minDepth topmPolyak, Boris GMinimum depth
7Temperature gradientT gradmK/mPolyak, Boris G
8Conductivity, averageCond averageW/m KPolyak, Boris G
9Heat FlowHFmW/m2Polyak, Boris G
10NumberNoPolyak, Boris GNumber of individual sites
11Method commentMethod commPolyak, Boris G
Size:
722 data points

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