File:Depth-Temperature relationship.png
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Summary
| Description |
English: Left: Heat-pipe tectonics develops a thicker and colder lithosphere by repetitive volcanic resurfacing. The lithosphere remains at low temperature, i.e. 600 degree Celsius, in great depth.
Right: Plate tectonics develops a thinner and hotter lithosphere that it raises to 1500 degree Celsius at shallow depth. |
| Date | |
| Source |
Moore, William B.; Webb, A. Alexander G. (2013). "Heat-pipe Earth". Nature. 501 (7468): 501–505. doi:10.1038/nature12473. ISSN 0028-0836. Arevalo, Ricardo; McDonough, William F.; Luong, Mario (2009-02). "The K/U ratio of the silicate Earth: Insights into mantle composition, structure and thermal evolution". Earth and Planetary Science Letters. 278 (3–4): 361–369. doi:10.1016/j.epsl.2008.12.023. ISSN 0012-821X. |
| Author |
Moore, William B.; Webb, A. Alexander G. Arevalo, Ricardo; McDonough, William F.; Luong, Mario |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 07:13, 12 November 2019 | | 2,224 × 987 (206 KB) | Kenwongtk | User created page with UploadWizard |
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