Talk:Litchfieldite

The genetic classification of Litchifieldite
There is no doubt that these rocks were affected by the metamorphism and this is the origin of some unique features present in litchfieldite: subsolvus paragenesis of feldspar, gnaissic and foliation, orientation of the nepheline optical axis, and so on. In some occurrence there was a certain grade of anatexis and the production of real igneous anatetic pgmatite, like in Canaã massif (Brazil).

I indicate in this case to adopt the same formula that was used to describe "Charnockite": metamorphosed igneous rocks.

I think that is the best way to satisfy the geologists who have difficulties to accept litchifieldite as metamorphic rock.

Zimbres 15:39, 26 March 2006 (UTC)

External links modified
Hello fellow Wikipedians,

I have just modified one external link on Litchfieldite. Please take a moment to review my edit. If you have any questions, or need the bot to ignore the links, or the page altogether, please visit this simple FaQ for additional information. I made the following changes:
 * Added archive https://web.archive.org/web/20150924021711/http://www.geologi.no/images/njg/1975-1979/1979/1/NGT_59_1_001-023.pdf to http://www.geologi.no/images/njg/1975-1979/1979/1/NGT_59_1_001-023.pdf

When you have finished reviewing my changes, you may follow the instructions on the template below to fix any issues with the URLs.

Cheers.— InternetArchiveBot  (Report bug) 15:59, 3 January 2018 (UTC)