Dear Dr. Parsapur,

the technical term "recrystallization" as applied to natural processes is self-explanatory in that a newly-crystallized phase comes into being which has a well-ordered crystalline state , reflected by certain lattic parameters. The way such a process can take place can be conducive to XX visible on a macroscopic scale and as such will obliterate the primordial state or goes the opposite way leading to microcrystalline XX which on a whole can presevere the outward appearance of the original state (e.g., micritisation). It strongly depends on the scale and angle you look at thischemical  system. Much of what we consider today a well-crystallized mineral is at risk of being sacked from this level as being viewed on a nano-scale. This is a more general approach taken which you can also apply to zeolites which often show up in nature as crusts, coatings and globular aggregates when viewed with the unarmed eye or under the hand lens. Using more advanced level techniques they are not at varaince to their analogues precipitated under different physical-chemical conditions.

Best regards

H.G.Dill

For more information you can find in book: Handbook of Zeolite Science and Technology.

All the best

S.Hyseni

Thank you Prof. Dill and Prof. Hyseni. Thanks for the term micritization.  Mechanism of zeolite crystallization indicates there is a dynamic equilibrium of bond breaking and forming between amorphous and crystalline phases, hence i am afraid there is a chance of restructuring of desired monolayer morphology to more stable 3D structure or other bulk structure. However the literature also suggests that crystallization of zeolite is mostly kinetically controlled. Hence I wanted to know synthesis conditions or probably a method by which i can crystallize monolayered amorphous sheets.

Thank you

 Tell me please?

Have you met in your practice aluminosilicates dendrimer morphology obtained by the sol-gel method from inorganic matter?

In the literature, I can not find the links.

Thanks in advance.