[Rockhounds] Mineral ID
Lawrence Rush
larryrush at worldnet.att.net
Sat Mar 8 07:05:53 PST 2008
Thanks very much, Andrew! Good answer!
Larry
-------------------------------------------------------------------
----- Original Message -----
From: "Andrew Turner" <turnea55 at hotmail.com>
To: <rockhounds at lists.drizzle.com>
Sent: Friday, March 07, 2008 8:19 PM
Subject: Re: [Rockhounds] Mineral ID
The lithium mica (e.g. lepidolite) phase diagram has something like 17
separate end members (I used it as a cover for a paper I did in phase
equilibria class). This means that there is technically some 17 different
dimensions to the diagram, good luck on the visualization and modelling. It
takes very little changes in temp., pressure, or chemsitry while the
mineral is forming to cause lithium (or any) mica to have a different color
and/or slightly varying chemisty, even to make it a separate species. This
is common for many pegmatite minerals due to how they form and how many of
them are "trash can" minerals in that they can accept numerous different
elements into their structures (check out the tourmaline or the
ferrocolumbite-manganotantalite series. Yellow, purple, and pink lepidolite
can be found together. I even have some pieces from South Dakota that are
half biotite and half muscovite (a small reaction zone of possible
phlogopite is seen at the contact). Hope this helps.
Andrew Turner
Victorville, CA USA
More information about the Rockhounds
mailing list