It is natural mineral but its photo-micrograph is not good, scince they are very small.
-------------------------
Dear Sobhi
First assumption before analysis, was Ortho-amphibole, because of paragenetic relations. But as Mattioli noticed, high Al vs lower Si in analysis, almost do not match to any amphiboles.
------------------------
Dear Mattioli
H2O is not available, but since total is about 98.5, some water is possible. I attached a SEM image, showing paragenesis and un-known (?) mineral.
I think the suggestion of Asoori is right, the mineralogical composition could represent a tourmaline group mineral. This is also supported by the associated minerals that can be seen in the SEM image: spinel + cordierite + sillimanite is a typical assemblage of metapelites and gneiss, and it is often associated with tourmaline and other phases.
See Darling et al. 2004, GSA Memoir 197: 325-336 as example.
I think it has too much Fe for a tourmaline, and normal tourmaline analyses close at ca. 87% wt%. Also, I don't believe that it is a tourmaline from the habit you show in the figure. Did you try new measurements? Is this the only attempt that you have made in this grain?
Thanks. I am thinking about Asoori's suggestion. Thanks for the chapter you mentioned.
But as Marta mentioned, the problem is high Fe and high total, comparing to normal tourmaline. As you see in Darling et al. 2004, about 10 % of B2O detected in their tourmaline. I do not have SIEMS analysis, but at least I think, total could be less than 90.
Of course, I am thinking about B-free tourmaline. But as you know, most of the tourmalines in metapelites, are metasomatic, there are rare metamorphic reactions discussing tourmaline. Proposed reaction in Darling et al. 2004, almost is impossible in this sample,
In this case, based on paragenesis, tourmaline in this sample could form during the reaction:
Spl+Crd= Tour + St
I think this reaction is possible, but needs more work.
So if this is really a tourmaline, then I should find a reaction. Of course, SIEMS could help, but for me is not available.
------------
Dear Marta
Thanks. I mentioned your comment in above part. Yes, could be problematic.
There are more than 10 analysis from different grains in the samples with more or less same composition. The analysis in my question, is average of 12 analysis and is not simple one.
I cannot access to the reference you're talking about, so I cannot give my own opinion about it. I can say for sure that you need 10-11 wt% B2O3 (3 apfu of B) to have tourmaline. Furthermore, I don't believe that there is such a thing as B-free tourmaline! If the mineral is B- free is not a tourmaline, because tourmaline is a boron-silicate.
It is probably an aluminous gedrite. Paragenesis is correct and the analysis is a little aluminous, but not the highest Al ever found by any means. The presence of a little Na is also typical.
Please check the attached file, calculated at the ends of possible Fe2+/Fe3+ ratios. I would bet on all Fe divalent. Withal, I'm so nostalgic of the times they used to make thin sections!
Why don't you use XRD to identify? XRD can identify the accurate mineral through diffraction pattern directly. Generally, it is not a smart method to determine the mineral name by using chemcial compositions.
First I should notice why thin section is not appropriate. the minerals are very thin and in association with other minerals like spinel and cordierite, form tiny symplectites. So their optical properties is not clear. and for the same reason, XRD doesn't work.
As I mentioned in previous notes, first guess was gedrite (Ortho-Amphibole). But Al was higher and, Si lower than normal. In Rock Forming Minerals (Chain Silicates) among many analysis, just one or two have more or less same composition.
Thanks For answers from Beard and Săbău.
I checked stoichiometry and almost all are Ferro-gedrite.