Abbott, Dallas H; Menke, William; Hobart, Michael A; Anderson, Roger N; Embley, Robert W (1984): Component parts of the World Heat Flow Data Collection [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.793492
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Abbott, Dallas H; Menke, William; Hobart, Michael A; Anderson, Roger N; Embley, Robert W (1984): Correlated sediment thickness, temperature gradient and excess pore pressure in a marine fault block basin. Geophysical Research Letters, 11(5), 485-488, https://doi.org/10.1029/GL011i005p00485
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
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: 10.077564 * Median Longitude: -90.494103 * South-bound Latitude: 9.941700 * West-bound Longitude: -90.987000 * North-bound Latitude: 10.210000 * East-bound Longitude: -90.003000
Minimum ELEVATION: -4016 m a.s.l. * Maximum ELEVATION: -3653 m a.s.l.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Area/locality | Area | Abbott, Dallas H | |||
2 | Sample, optional label/labor no | Lab no | Abbott, Dallas H | Site name | ||
3 | LATITUDE | Latitude | Geocode | |||
4 | LONGITUDE | Longitude | Geocode | |||
5 | ELEVATION | Elevation | m a.s.l. | Geocode | ||
6 | Depth, top/min | Depth top | m | Abbott, Dallas H | Minimum depth | |
7 | Depth, bottom/max | Depth bot | m | Abbott, Dallas H | Maximum depth | |
8 | Number of temperature data | No Temps | Abbott, Dallas H | |||
9 | Temperature gradient | T grad | mK/m | Abbott, Dallas H | ||
10 | Conductivity, average | Cond average | W/m K | Abbott, Dallas H | ||
11 | Heat flow | HF | mW/m2 | Abbott, Dallas H | ||
12 | Number | No | Abbott, Dallas H | Number of individual sites | ||
13 | Method comment | Method comm | Abbott, Dallas H |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
351 data points
Data
1 Area | 2 Lab no | 3 Latitude | 4 Longitude | 5 Elevation [m a.s.l.] | 6 Depth top [m] | 7 Depth bot [m] | 8 No Temps | 9 T grad [mK/m] | 10 Cond average [W/m K] | 11 HF [mW/m2] | 12 No | 13 Method comm |
---|---|---|---|---|---|---|---|---|---|---|---|---|
Pacific Ocean | END48-4B | 10.2100 | -90.010 | -3710 | 1 | 4 | 3 | 0.60 | 91 | 1 | ||
Pacific Ocean | END48-7B | 10.0467 | -90.410 | -3863 | 1 | 5 | 3 | 100 | 0.60 | 60 | 1 | |
Pacific Ocean | END48-7E | 9.9833 | -90.440 | -3829 | 1 | 5 | 4 | 97 | 0.60 | 59 | 1 | |
Pacific Ocean | END48-7C | 10.0017 | -90.388 | -3857 | 1 | 5 | 4 | 89 | 0.60 | 54 | 1 | |
Pacific Ocean | END48-7D | 10.0000 | -90.403 | -3857 | 1 | 5 | 4 | 89 | 0.60 | 54 | 1 | |
Pacific Ocean | END48-7F | 9.9683 | -90.472 | -3818 | 1 | 5 | 4 | 87 | 0.60 | 52 | 1 | |
Pacific Ocean | END48-6F | 10.0633 | -90.423 | -3797 | 2 | 5 | 4 | 84 | 0.60 | 50 | 1 | |
Pacific Ocean | END48-6E | 10.0733 | -90.402 | -3812 | 1 | 5 | 5 | 82 | 0.60 | 49 | 1 | |
Pacific Ocean | END48-4A | 10.2100 | -90.003 | -3701 | 1 | 5 | 5 | 77 | 0.60 | 46 | 1 | |
Pacific Ocean | END48-6C | 10.0950 | -90.332 | -3860 | 1 | 5 | 5 | 73 | 0.60 | 44 | 1 | |
Pacific Ocean | END48-4D | 10.2050 | -90.080 | -3676 | 1 | 3 | 2 | 69 | 0.60 | 42 | 1 | |
Pacific Ocean | END48-7A | 10.0567 | -90.398 | -3863 | 1 | 5 | 3 | 61 | 0.60 | 37 | 1 | |
Pacific Ocean | END48-4G | 10.1700 | -90.207 | -3965 | 1 | 5 | 5 | 53 | 0.68 | 36 | 1 | |
Pacific Ocean | END48-6D | 10.0867 | -90.358 | -3834 | 2 | 5 | 4 | 59 | 0.60 | 36 | 1 | |
Pacific Ocean | END48-6A | 10.1350 | -90.312 | -3853 | 1 | 5 | 5 | 56 | 0.60 | 34 | 1 | |
Pacific Ocean | END48-2I | 9.9817 | -90.987 | -3752 | 1 | 5 | 5 | 49 | 0.60 | 30 | 1 | |
Pacific Ocean | END48-4C | 10.2083 | -90.045 | -3653 | 1 | 5 | 5 | 44 | 0.60 | 26 | 1 | |
Pacific Ocean | END48-2G | 10.0267 | -90.923 | -3739 | 1 | 4 | 4 | 43 | 0.60 | 26 | 1 | |
Pacific Ocean | END48-6B | 10.1100 | -90.328 | -3860 | 1 | 5 | 5 | 41 | 0.60 | 25 | 1 | |
Pacific Ocean | END48-2H | 9.9950 | -90.965 | -3755 | 2 | 5 | 4 | 41 | 0.60 | 25 | 1 | |
Pacific Ocean | END48-5 | 10.0833 | -90.483 | -3802 | 2 | 14 | 5 | 40 | 0.61 | 24 | 1 | |
Pacific Ocean | END48-4H | 10.1350 | -90.245 | -3913 | 1 | 4 | 4 | 32 | 0.60 | 19 | 1 | |
Pacific Ocean | END48-1A | 10.0883 | -90.633 | -3777 | 1 | 5 | 4 | 28 | 0.60 | 17 | 1 | BHT |
Pacific Ocean | END48-1F | 10.0000 | -90.697 | -3720 | 1 | 5 | 4 | 27 | 0.60 | 16 | 1 | |
Pacific Ocean | END48-4E | 10.2033 | -90.150 | -4013 | 1 | 5 | 4 | 22 | 0.68 | 15 | 1 | |
Pacific Ocean | END48-7G | 9.9517 | -90.537 | -3822 | 1 | 5 | 4 | 24 | 0.60 | 15 | 1 | |
Pacific Ocean | END48-1B | 10.0700 | -90.640 | -3769 | 1 | 5 | 4 | 23 | 0.60 | 14 | 1 | |
Pacific Ocean | END48-4F | 10.1867 | -90.172 | -4000 | 1 | 5 | 5 | 20 | 0.68 | 14 | 1 | |
Pacific Ocean | END48-2F | 10.0333 | -90.878 | -3973 | 2 | 5 | 4 | 21 | 0.60 | 13 | 1 | |
Pacific Ocean | END48-2A | 10.1283 | -90.687 | -3721 | 1 | 5 | 5 | 21 | 0.60 | 13 | 1 | |
Pacific Ocean | END48-3 | 10.0583 | -90.763 | -3855 | 2 | 8 | 4 | 19 | 0.66 | 12 | 1 | |
Pacific Ocean | END48-1C | 10.0650 | -90.640 | -3779 | 2 | 5 | 3 | 18 | 0.60 | 11 | 1 | |
Pacific Ocean | END48-2B | 10.1217 | -90.695 | -3699 | 2 | 5 | 4 | 17 | 0.60 | 10 | 1 | |
Pacific Ocean | END48-7H | 9.9417 | -90.538 | -3831 | 1 | 5 | 4 | 16 | 0.60 | 10 | 1 | |
Pacific Ocean | END48-1E | 10.0333 | -90.688 | -3744 | 2 | 5 | 3 | 15 | 0.60 | 9 | 1 | |
Pacific Ocean | END48-1D | 10.0467 | -90.655 | -3784 | 2 | 5 | 3 | 13 | 0.60 | 8 | 1 | |
Pacific Ocean | END48-2C | 10.1133 | -90.730 | -3671 | 1 | 5 | 5 | 9 | 0.60 | 5 | 1 | |
Pacific Ocean | END48-2D | 10.0717 | -90.753 | -3693 | 2 | 5 | 4 | 9 | 0.60 | 5 | 1 | |
Pacific Ocean | END48-2E | 10.0667 | -90.800 | -4016 | 2 | 5 | 4 | 6 | 0.60 | 4 | 1 |