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Stubbed this because: Need more links on the ophiolite complexes; need some thumbnail maps of the ophiolites as well as images, sections, etc. Rolinator 14:47, 26 January 2006 (UTC)
The majority of SSZ ophiolites now appear to be regarded as the result of subduction rollback in the literature, in order to produce the local extension regieme in an overall compressive setting. No seperate topic on rollback itself, subduction section is in need of improvement as well, currently working on a new graphic for that one which might be upload in the next couple of weeks. Will try and update the ophiolite formation section once I've got to grips with the wiki style of writing. ClimberDave 13:47, 17 April 2007 (UTC)
Is it worth adding another image? I dont think this image below is too great but it better shows the dyke/lava relationship MeanStreets "...Chorizo..." 12:34, 28 April 2007 (UTC)
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@ Mamayuco: You added {{ dubious}} to the statement about Macquarie Island. I checked out the reference given—it turned out that the statement was a direct quote from the source, so I've removed the template (and added quote marks so it's not a copyright violation!). Please feel free to reword it if you feel it needs to be, but be sure to cite your sources. Cheers! — Gorthian ( talk) 18:19, 28 April 2016 (UTC)
The recent removal of the longstanding uncited sections about, amongst other things, ophiolites in the alps got me thinking. I've recently been working on passive margins using the models of Gianreto Manatschal and his colleagues, who base a lot of their understanding of magma-poor passive margins on exposures from the Alps. These Alpine ophiolites are unusual (see e.g. Manatschal & Müntener 2009) so at least the first of the deleted paragraphs doesn't look that far off the mark. I'm not suggesting putting the deleted text back, just that we should probably have a section on the Alpine ophiolites and their interpretation. Mikenorton ( talk) 15:56, 9 March 2018 (UTC)
![]() | This article is rated B-class on Wikipedia's
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Stubbed this because: Need more links on the ophiolite complexes; need some thumbnail maps of the ophiolites as well as images, sections, etc. Rolinator 14:47, 26 January 2006 (UTC)
The majority of SSZ ophiolites now appear to be regarded as the result of subduction rollback in the literature, in order to produce the local extension regieme in an overall compressive setting. No seperate topic on rollback itself, subduction section is in need of improvement as well, currently working on a new graphic for that one which might be upload in the next couple of weeks. Will try and update the ophiolite formation section once I've got to grips with the wiki style of writing. ClimberDave 13:47, 17 April 2007 (UTC)
Is it worth adding another image? I dont think this image below is too great but it better shows the dyke/lava relationship MeanStreets "...Chorizo..." 12:34, 28 April 2007 (UTC)
Hello fellow Wikipedians,
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Ophiolite. Please take a moment to review
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An editor has reviewed this edit and fixed any errors that were found.
Cheers. — cyberbot II Talk to my owner:Online 14:08, 17 October 2015 (UTC)
Hello fellow Wikipedians,
I have just added archive links to one external link on
Ophiolite. Please take a moment to review
my edit. If necessary, add {{
cbignore}}
after the link to keep me from modifying it. Alternatively, you can add {{
nobots|deny=InternetArchiveBot}}
to keep me off the page altogether. I made the following changes:
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Cheers.— cyberbot II Talk to my owner:Online 03:41, 28 February 2016 (UTC)
@ Mamayuco: You added {{ dubious}} to the statement about Macquarie Island. I checked out the reference given—it turned out that the statement was a direct quote from the source, so I've removed the template (and added quote marks so it's not a copyright violation!). Please feel free to reword it if you feel it needs to be, but be sure to cite your sources. Cheers! — Gorthian ( talk) 18:19, 28 April 2016 (UTC)
The recent removal of the longstanding uncited sections about, amongst other things, ophiolites in the alps got me thinking. I've recently been working on passive margins using the models of Gianreto Manatschal and his colleagues, who base a lot of their understanding of magma-poor passive margins on exposures from the Alps. These Alpine ophiolites are unusual (see e.g. Manatschal & Müntener 2009) so at least the first of the deleted paragraphs doesn't look that far off the mark. I'm not suggesting putting the deleted text back, just that we should probably have a section on the Alpine ophiolites and their interpretation. Mikenorton ( talk) 15:56, 9 March 2018 (UTC)