Monday, June 13, 2011

Rethinking Heat Transport (Was:[Geology2] Mag. 6.0 earthquake, Canterbury region, New Zealand)

http://www.sciencemag.org/content/332/6033/1068
http://news.sciencemag.org/sciencenow/2011/05/another-look-beneath-hawaii-knoc.html?rss=1

The above two articles, probably, let us rethink current mantle plumes
and convection.concept. I tried to suggest another
heat transport mechanism:

Tectonics. Types Of Heat Transport To Develop Calderas, Volcanoes, And
Divergent Boundaries.
http://divergent-boundaries.blogspot.com/2011/06/tectonics-types-of-heat-transport-to.html

Sergey Sukhotinsky.

---
Slow Earthquake In Case A Divergent Boundary Is Close To Subduction Zone.
http://divergent-boundaries.blogspot.com/2011/06/slow-earthquakes.html

Formation Of Mountain Ridges by Broken Process Of Subduction Of A
Tectonic Plate.
http://divergent-boundaries.blogspot.com/2011/05/mountain-ridges-formation-keeping-it.html

On Mon, Jun 13, 2011 at 6:15 AM, Lin Kerns <linkerns@gmail.com> wrote:
>
>
>
>                    PRELIMINARY EARTHQUAKE REPORT
>
>                             GNS SCIENCE
>                          GeoNet Data Centre
>                       Lower Hutt, New Zealand
>                       http://www.geonet.org.nz
>
>
>        The following earthquake has been recorded by GNS Science:
>
>        Reference number:        3528839/G
>        Universal Time:          13 June 2011 at 02:20
>        NZ Standard Time:        Monday, 13 June 2011 at 2:20 pm
>        Latitude, Longitude:     43.58°S, 172.74°E
>        Location:                10 km south-east of Christchurch
>        Focal depth:             9 km
>        Richter magnitude:       6.0
>
>        Web page: http://www.geonet.org.nz/earthquake/quakes/3528839g.html
>
> Felt widely in Canterbury.
>
>
> The GeoNet project is core funded by the Earthquake Commission (EQC) and is
> being designed, installed and operated by GNS Science on behalf of EQC and all
> New Zealanders.
>


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