[Rockhounds] Scapolite
DonH
donhalterman at verizon.net
Tue Sep 23 19:00:18 PDT 2008
Axel Emmermann wrote:
> That is why I would like to know whether there is a noticeable discrepancy
> between the occurrence of large, gemmy crystals of both species or that it's
> apparently not a big deal ;-)
Well, Pete Richards would be a better person to give a definitive answer
on this exact question. As I mentioned previously, the main driving
factors in crystal growth are the composition of the melt and rates of
cooling.
To quote my advanced mineralogy professor, most minerals at the
nano-scale are a mess; full of defects, dislocations, and substitutions.
We studied tourmalines, apatites, and feldspars, among other
important minerals,and one wonders how these ever form recongizable
crystals at all, given everything that can go wrong during their
formation. Yet they do. There is a big difference between what happens
on the molecular scale and the macro scale. Feldspars in particular are
an atomic game of musical chairs, followed by outright molecular warfare
as they cool and try to form stable structures. Yet, again, we see
beautiful, sharp, and well-formed large crystals of these. If you look
closely at many of them, you can see the exsolution lamellae where the
incompatible entities separated; yet, on the hand scale, the crystal can
still have a perfect morphology.
> It seems also that the ratio of Al-occupied/Si-occupied tetrahedrons is much
> higher in meionite than in marialite. Something in the order of 10 to 15 %
> more Al than Si. Does this mean that Fe3+ substituting for Al could also
> occur more frequently in meionite than in marialite?
That's easier to answer: Fe3+ will often substitute for Al3+, depending
of course on the size of the coordination polyhedra. However, there is
a limit to the degree of substitution that will actually occur. Si and
Al have high surface charges and they like to grab the free oxygens
first; and, since O, Si, and Al are the most abundant elements before
Fe, it makes sense that there will be more Si-O and Al-O polyanions in
the average melt (with "average" being the operative word; plenty of
exceptions there, of course).
Well, I am moving to take my new job, so I won't be writing much in the
next few weeks. I'm also hoping someone with more knowledge and
experience on the subject will have a more suitable answer.
best,
Don
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