Sclater, John G (1966): Component parts of the World Heat Flow Data Collection [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.805893
Always quote citation above when using data! You can download the citation in several formats below.
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), https://ihfc-iugg.org/products/global-heat-flow-database/data
Sclater, John G (1966): Heat Flow in the Northwest Indian Ocean and Red Sea. Philosophical Transactions of the Royal Society of London Series A-Mathematical and Physical Sciences, 259(1099), 271-278, https://doi.org/10.1098/rsta.1966.0012
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: 2.199354 * Median Longitude: 50.481469 * South-bound Latitude: -6.650000 * West-bound Longitude: 39.783300 * North-bound Latitude: 18.400000 * East-bound Longitude: 61.951700
Minimum ELEVATION: -5100 m a.s.l. * Maximum ELEVATION: -1480 m a.s.l.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample, optional label/labor no | Lab no | Sclater, John G | |||
2 | LATITUDE | Latitude | Geocode | |||
3 | LONGITUDE | Longitude | Geocode | |||
4 | ELEVATION | Elevation | m a.s.l. | Geocode | ||
5 | Temperature gradient | T grad | mK/m | Sclater, John G | ||
6 | Conductivity, average | Cond average | W/m K | Sclater, John G | ||
7 | Heat flow | HF | mW/m2 | Sclater, John G | ||
8 | Number | No | Sclater, John G | Number of individual sites | ||
9 | Method comment | Method comm | Sclater, John G |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
155 data points
Data
1 Lab no | 2 Latitude | 3 Longitude | 4 Elevation [m a.s.l.] | 5 T grad [mK/m] | 6 Cond average [W/m K] | 7 HF [mW/m2] | 8 No | 9 Method comm |
---|---|---|---|---|---|---|---|---|
DIS-5116 | 5.5833 | 61.9517 | -3560 | 66 | 0.85 | 56 | 1 | |
DIS-5122 | 5.5833 | 61.9333 | -3560 | 64 | 0.84 | 54 | 1 | Ewing probe |
DIS-5125 | 2.7500 | 60.2500 | -4806 | 26 | 0.71 | 19 | 1 | Ewing probe |
DIS-5135 | 2.9167 | 59.8833 | -4697 | 41 | 0.74 | 31 | 1 | Ewing probe |
DIS-5139 | 1.9000 | 56.1667 | -4812 | 73 | 0.72 | 53 | 1 | Ewing probe |
DIS-5144 | -1.6833 | 42.2167 | -2255 | 70 | 0.84 | 59 | 1 | Ewing probe |
DIS-5149 | -2.4000 | 43.4000 | -3552 | 64 | 0.82 | 53 | 1 | Ewing probe |
DIS-5152 | -2.5333 | 44.9333 | -4160 | 62 | 0.78 | 48 | 1 | Ewing probe |
DIS-5155 | -2.8000 | 47.0500 | -4812 | 61 | 0.74 | 45 | 1 | Ewing probe |
DIS-5160 | -3.5000 | 49.6667 | -5042 | 72 | 0.74 | 54 | 1 | Ewing probe |
DIS-5165 | -3.5500 | 51.4833 | -5100 | 42 | 0.71 | 30 | 1 | Ewing probe |
DIS-5171 | -2.1667 | 57.4167 | -4402 | 22 | 0.95 | 21 | 1 | Ewing probe |
DIS-5177 | -2.2000 | 57.3333 | -4402 | 52 | 0.89 | 46 | 1 | Ewing probe |
DIS-5180 | -6.6500 | 54.2667 | -3824 | 75 | 0.86 | 65 | 1 | Ewing probe |
DIS-5190 | -2.8500 | 47.0000 | -4800 | 66 | 0.76 | 50 | 1 | Ewing probe |
DIS-5194 | -2.5667 | 44.8833 | -4180 | 60 | 0.80 | 48 | 1 | Ewing probe |
DIS-5201 | -1.7000 | 42.2500 | -2046 | 61 | 0.85 | 52 | 1 | Ewing probe |
DIS-5204 | -3.5167 | 48.3833 | -4940 | 76 | 0.75 | 57 | 1 | Ewing probe |
DIS-5207 | -3.5667 | 50.4833 | -5082 | 71 | 0.77 | 54 | 1 | Ewing probe |
DIS-5215 | -2.4167 | 54.7500 | -4360 | 75 | 0.84 | 63 | 1 | Ewing probe |
DIS-5226 | 11.1167 | 54.0500 | -4028 | 75 | 0.87 | 65 | 1 | Ewing probe |
DIS-5227 | 11.6500 | 47.8333 | -1900 | 180 | 0.90 | 161 | 1 | Ewing probe |
DIS-5229 | 12.4833 | 47.0333 | -2197 | 269 | 0.96 | 258 | 1 | Ewing probe |
DIS-5230 | 12.9333 | 46.6000 | -1600 | 150 | 0.90 | 136 | 1 | Ewing probe |
DIS-5231 | 15.9667 | 41.5167 | -1735 | 181 | 0.97 | 175 | 1 | Ewing probe |
DIS-5232 | 18.4000 | 39.7833 | -1480 | 40 | 1.10 | 44 | 1 | Ewing probe |