Talk:Large low-shear-velocity provinces
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This article was the subject of an educational assignment in Spring 2015. Further details were available on the "Education Program:University of North Alabama/480 Geotectonics (Spring 2015)" page, which is now unavailable on the wiki. |
I can't find much on the discovery, and wiki won't let me add charts(copyright). Seeing that LLSVPs are the driving force behind plate tectonics the information it would seem is understandably useful. And I hope what I added to the spherical harmonics section helps clear up how its related.Losgrinch30 (talk) 03:14, 5 May 2015 (UTC)
I like your page! You have some great information on here! Maybe you could add a little about the discovery of the LLSVP and something about how knowing about these areas helps seismology in some way. Mhunter2 (talk) 01:29, 21 April 2015 (UTC)
I agree with Maisey, how can this information be useful, not just in seismology but in general? Someone was studying it for a reason, right? Also, since it is something characterized by wave velocity, is there a way to have a diagram or graph showing how the shear velocity changes in these areas? Other than that, very nice article. Really neat structures. NealeyS (talk) 14:15, 24 April 2015 (UTC)
In the seismological constraints section, how does the strength of the spherical harmonic relate to the seismic constraints on these structures?Mcooper3 (talk) 02:52, 25 April 2015 (UTC)
I think your page is good. You have good information and nice pictures! I don't find any problem from your page. Tomoyuki6 (talk) 22:42, 27 April 2015 (UTC)
Edits
editFirst paragraph: i don't think they are AKA superplumes and superwells. I'd love to know more about the "seduction" zones!! :) (under Possible Origins). Isn't there a page on ULVZ. link to it. Have you linked other pages to yours? Mmdriskell (talk) 16:01, 5 May 2015 (UTC) Anisotropy?Mmdriskell (talk) 16:02, 5 May 2015 (UTC)
Histoy.
editWhat, when, how, whom? To differentiate from science to comic. 1.47.156.241 (talk) 12:34, 6 November 2023 (UTC)