Role of tetrabutylammonium bromide in formation of structure of high-silica zeolite TsVK-1

1986 ◽  
Vol 22 (5) ◽  
pp. 234-236 ◽  
Author(s):  
G. D. Chukin ◽  
B. L. Khusid ◽  
G. V. Vasilenko ◽  
G. B. Belan
2015 ◽  
Vol 51 (49) ◽  
pp. 9965-9968 ◽  
Author(s):  
Nuria Martín ◽  
Manuel Moliner ◽  
Avelino Corma

The synthesis of chabazite with high solid yields is achieved by the rational combination of directing effects of a source of Si and Al coming from USY zeolites and the inexpensive tetraethylammonium.


2007 ◽  
Vol 101 (1-2) ◽  
pp. 153-160 ◽  
Author(s):  
B. Bonelli ◽  
L. Forni ◽  
A. Aloise ◽  
J.B. Nagy ◽  
G. Fornasari ◽  
...  

2020 ◽  
Author(s):  
Aniruddha Mitra ◽  
Sukanta Dey ◽  
Keqing Zong ◽  
Yongsheng Liu ◽  
Anirban Mitra

<p>Singhbhum Craton, eastern India, exposes some of the oldest known composite Paleoarchean granitoids. These granitoids range from sodic TTGs to evolved, potassic granites.  The whole process of their formation, starting from nucleation of a juvenile continent to its evolution and final stabilization is documented. The central part of the craton started nucleating with the formation of 3.45–3.40Ga juvenile (zircon εHf<sub>t</sub>=+0.6 to +7.1) TTGs. These TTGs characterized by slightly depleted HREE and Y, negligible Eu-anomaly (Eu/Eu*=0.90 to 1.00) and moderate Sr/Y (25–64), consistent with derivation from a low-K mafic crust at a pressure near the lower end of the garnet stability field, causing subordinate garnet retention in the residue and negligible role of plagioclase. During 3.32Ga, deeper melting of a juvenile mafic crust (zircon εHf<sub>t</sub>=+1.3 to +5.7) caused emplacement of a second generation of TTG. Deeper melting is suggested by depleted HREE and Y, and high Sr/Y (52–155), implying significant amount of residual garnet retention. Subsequently at 3.28 and 3.25Ga, melting of moderately old to juvenile (zircon εHf<sub>t</sub>=-1.9 to +4.5), mostly TTG sources at variable depths generated potassic, LILE-enriched, high-silica granites. Intrusion of these potassic granites resulted in a stable and buoyant crust that marked the final Cratonization of the Singhbhum Craton. The sequence of events is interpreted in terms of repeated intracrustal melting and granitoid generation in a gradually thickening oceanic plateau with a progressive change in granitoid source from mafic to felsic in composition. Combination of rock assemblage, regional geology, and structural pattern also supports intraplate nature of the magmatism in Singhbhum Craton, which might have been a significant mechanism of crustal growth worldwide during Paleoarchean.</p>


2008 ◽  
Vol 422 (1) ◽  
pp. 240-243 ◽  
Author(s):  
A. L. Lapidus ◽  
M. N. Mikhailov ◽  
A. A. Dergachev ◽  
I. V. Mishin

2012 ◽  
Vol 116 (12) ◽  
pp. 6943-6952 ◽  
Author(s):  
Ilaria Braschi ◽  
Giorgio Gatti ◽  
Chiara Bisio ◽  
Gloria Berlier ◽  
Vittoria Sacchetto ◽  
...  

1986 ◽  
Vol 86 ◽  
Author(s):  
F. P. Glasser ◽  
S. Diamond ◽  
D. M. Roy

ABSTRACTA model for reactions that occur in hydrating portland cement is now generally well developed. Incorporation of various by-products to form blended cements modifies both the hydration reactions and the physical properties of the resulting pastes. A review of recent progress in understanding the effects of blending agents on these reactions is presented. The blending agents considered are low-calcium (Class F) fly ash, high calcium (Class C) fly ash, blast furnace slag, silica fume, biosilica and natural pozzolans. Effects of the blending agents on physical properties such as rheology are also considered. Particular attention is given to the essential role of alkalies in pore solutions and the beneficial reactions that occur with high silica content blending agents.


Author(s):  
Kh. M. Minachev ◽  
D. A. Kondrat'ev ◽  
A. L. Klyachko ◽  
A. Yu. Borodkin ◽  
G. O. Glonti ◽  
...  

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