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Science

Volumn 320, Issue 5881, 2008, Pages

Response to comment on "intermittent plate tectonics?"

(2) Silver, Paul G a Behn, Mark D b

a GEOPHYSICAL LABORATORY (United States)

b WOODS HOLE OCEANOGRAPHIC INSTITUTION (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CALCULATION; DISASTER; GEOGRAPHIC AND GEOLOGICAL PHENOMENA; HEAT TRANSFER; LITHOSPHERE; MATHEMATICAL ANALYSIS; NOTE; PLATE TECTONICS; PRIORITY JOURNAL; PROTEROZOIC; TEMPERATURE SENSITIVITY; THERMAL CONDUCTIVITY; THICKNESS; TIME;

EID: 46449104039 PISSN: 00368075 EISSN: 10959203 Source Type: Journal
DOI: 10.1126/science.1155338 Document Type: Note

Times cited : (4)

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- Assuming HSC, we define the areally averaged heat flux for a pre-existing ocean basin as ∫q(τ(r, dr/∫dr, where r is the distance from the ridge axis and τ is the age of the sea floor at distance r when plate tectonics stops. For a constant spreading velocity, V, τ, r/V, and τ ranges from 0 to the oldest sea floor, τmax. can then be expressed in terms of τmax and the time, t, subsequent to the cessation of plate tectonics as < q >= Cτ max-1 ∫0τmax (τ, t)-1/2 dτ, where C, kΔT (πκ)-1/2, k is thermal conductivity (3.2 WmK -1, ΔT is the temperature contrast between surface and interior (1350 K, and κ is the thermal diffusivity 10-6 m/s, Inte
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- We thank C. Conrad, R. Buck, and four anonymous reviewers. This work is supported by the Department of Terrestrial Magnetism, Carnegie Institution of Washington, and the Woods Hole Oceanographic Institution
- We thank C. Conrad, R. Buck, and four anonymous reviewers. This work is supported by the Department of Terrestrial Magnetism, Carnegie Institution of Washington, and the Woods Hole Oceanographic Institution.

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