“…Y mutinaite, as above, Y tschernichite, the Al-bearing analog of the Mobil high silica zeolite Beta (59-67), which has a remarkable polytypic domain structure with a 10-ring, three-dimensional channel system, Y boggsite, with a 10-to 12-ring, three-dimensional channel system, which occurs with tschernichite in Columbia basalt (68), Y faujasite, the natural analog of Linde Type Y, the main industrial catalyst with a 12-ring, three-dimensional channel system; can be de-aluminated by various processes (not referenced in detail); known only as a very rare mineral until discovery in sedimentary beds of diagenetic tuffs in Jordan (69), Y mordenite, an easily de-aluminated, common, high silica natural zeolite, with industrial analogs, whose one-dimensional channel can be blocked by either faulting or an Al-complex , Y mesoporous silicas with nanometer channels and mainly hydrophilic surfaces but some organophilic behavior (91)(92)(93)(94)(95)(96)(97)(98)(99)(100)(101)(102)(103), Y all-silica analog (Chevron SSZ-24) of Union Carbide aluminophosphate AlPO-5, for which one might envisage unipolar segments of aluminophosphate interleaved with nonpolar silica down the 12-ring cylindrical channel (104)(105), and Y theoretical chiral frameworks in the database of the Consortium for Theoretical Frameworks, University of Chicago, being prepared for publication.…”