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To: Renfield

According to this revelation, when a plate sinks well into the abyss of the earth’s core, down 1,200 miles; it retains some of the original structure it had when it was close to the surface. I would have assumed it would have been disolved by then.

The climate and typography assumptions of the Jurassic and earlier remain.


5 posted on 04/17/2013 7:25:24 AM PDT by cicero2k
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To: cicero2k
I think what they're looking at is the accretionary wedge at the upper limit of the subduction zone. What they are saying is that rather than than a single subduction zone along the margin of the NA plate, there was also westward movement (from the Juan de Fuca/Farallon spreading center) that accounted for another “left-handed” subduction zone further west that is now being overridden by the NA plate.
7 posted on 04/17/2013 7:39:36 AM PDT by stormer
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To: cicero2k
According to this revelation, when a plate sinks well into the abyss of the earth’s core, down 1,200 miles; it retains some of the original structure it had when it was close to the surface. I would have assumed it would have been disolved by then.

This has been a result of new discoveries, understanding, and modeling over the past decade or so.

I think it's pretty widely believed that subducted slabs are actually hitting the core-mantle boundary, astonishingly.

8 posted on 04/17/2013 7:45:27 AM PDT by Strategerist
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To: cicero2k

“I would have assumed it would have been disolved by then.”

Yeah! Cuz it’s, like, millions of degrees down there right? Somebody said that.
8^)


9 posted on 04/17/2013 7:48:03 AM PDT by Dr. Bogus Pachysandra ( Ya can't pick up a turd by the clean end!)
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