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	<title>Comments on: Aaand, the rest of AGU</title>
	<atom:link href="http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/feed/" rel="self" type="application/rss+xml" />
	<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/</link>
	<description>rock out to the apparatus</description>
	<pubDate>Thu, 29 Jul 2010 20:30:26 +0000</pubDate>
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		<title>By: Belize</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-27343</link>
		<dc:creator>Belize</dc:creator>
		<pubDate>Tue, 29 Jan 2008 22:30:47 +0000</pubDate>
		<guid isPermaLink="false">http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-27343</guid>
		<description>No, nothing to do with Kippers Beatrice.  Andy has the right idea above.  I've heard he is a world expert on this stuff.</description>
		<content:encoded><![CDATA[<p>No, nothing to do with Kippers Beatrice.  Andy has the right idea above.  I&#8217;ve heard he is a world expert on this stuff.</p>
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		<title>By: Beatrice</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-27342</link>
		<dc:creator>Beatrice</dc:creator>
		<pubDate>Tue, 29 Jan 2008 22:20:46 +0000</pubDate>
		<guid isPermaLink="false">http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-27342</guid>
		<description>Does foundering have anything to do with the discovery of kippers in the ocean off the coast of the W USA near the Sierra Nevada?</description>
		<content:encoded><![CDATA[<p>Does foundering have anything to do with the discovery of kippers in the ocean off the coast of the W USA near the Sierra Nevada?</p>
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		<title>By: Andy Frassetto</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-25326</link>
		<dc:creator>Andy Frassetto</dc:creator>
		<pubDate>Mon, 07 Jan 2008 20:52:58 +0000</pubDate>
		<guid isPermaLink="false">http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-25326</guid>
		<description>We like to think of delamination as a more brittle or seismogenic process (e.g. the deep crustal earthquakes under the western Sierra foothills or the Vrancea zone in Romania). An R-T instability, in addition to having different morphology criteria for initiation, is considered a lot more ductile.

I like this blog!</description>
		<content:encoded><![CDATA[<p>We like to think of delamination as a more brittle or seismogenic process (e.g. the deep crustal earthquakes under the western Sierra foothills or the Vrancea zone in Romania). An R-T instability, in addition to having different morphology criteria for initiation, is considered a lot more ductile.</p>
<p>I like this blog!</p>
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		<title>By: Lab Lemming</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23996</link>
		<dc:creator>Lab Lemming</dc:creator>
		<pubDate>Thu, 20 Dec 2007 04:23:02 +0000</pubDate>
		<guid isPermaLink="false">http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23996</guid>
		<description>I thought delamination was the loss of strength in between the two layers, and foundering was the sinking that happens once the lower one realizes that nothing is holding it up anymore (a.k.a. Wile E. Coyote)</description>
		<content:encoded><![CDATA[<p>I thought delamination was the loss of strength in between the two layers, and foundering was the sinking that happens once the lower one realizes that nothing is holding it up anymore (a.k.a. Wile E. Coyote)</p>
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		<title>By: yami</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23955</link>
		<dc:creator>yami</dc:creator>
		<pubDate>Wed, 19 Dec 2007 07:02:32 +0000</pubDate>
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		<description>I always think of foundering as the generic process of falling off, and delamination as a particular way of doing it where the lower lithosphere peels off as a coherent sheet - which is different from, say, foundering via Rayleigh-Taylor instability ("deblobbing"). I think some people also use delamination as a generic term, but I am so fond of the word "deblobbing" that I prefer to maintain the distinction.</description>
		<content:encoded><![CDATA[<p>I always think of foundering as the generic process of falling off, and delamination as a particular way of doing it where the lower lithosphere peels off as a coherent sheet - which is different from, say, foundering via Rayleigh-Taylor instability (&#8221;deblobbing&#8221;). I think some people also use delamination as a generic term, but I am so fond of the word &#8220;deblobbing&#8221; that I prefer to maintain the distinction.</p>
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		<title>By: Andrew Alden</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23952</link>
		<dc:creator>Andrew Alden</dc:creator>
		<pubDate>Wed, 19 Dec 2007 04:00:01 +0000</pubDate>
		<guid isPermaLink="false">http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23952</guid>
		<description>Yes, they're the same process. The lithosphere has to delaminate first before it can founder, though.</description>
		<content:encoded><![CDATA[<p>Yes, they&#8217;re the same process. The lithosphere has to delaminate first before it can founder, though.</p>
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		<title>By: Kim</title>
		<link>http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23907</link>
		<dc:creator>Kim</dc:creator>
		<pubDate>Tue, 18 Dec 2007 14:21:20 +0000</pubDate>
		<guid isPermaLink="false">http://greengabbro.net/2007/12/17/aaand-the-rest-of-agu/#comment-23907</guid>
		<description>Is lithospheric foundering essentially the same thing as lithospheric delamination? (When I've seen talks discussing one or the other, I tend to equate them, but maybe I shouldn't.)</description>
		<content:encoded><![CDATA[<p>Is lithospheric foundering essentially the same thing as lithospheric delamination? (When I&#8217;ve seen talks discussing one or the other, I tend to equate them, but maybe I shouldn&#8217;t.)</p>
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