Two feldspars of composition Ca0.3Sr0.7Al2Si2O8 (An30SrF70) and Ca0.6Sr0.4Al2Si2O8 (An60SrF40) were synthesized from gel and annealed at temperatures between 1150 and 1480{degrees}C for durations between 0.025 (1.5 min) and 1073 h. The An60SrF40 feldspar is triclinic for all annealing temperatures, whereas the An30SrF70 possesses, at room temperature, a monoclinic symmetry, C2/m in the shortest annealing runs and I2/c after slightly longer heating, and becomes triclinic after prolonged annealing. A TTT plot for the triclinic-monclinic transition shows an activation energy of 101{+/-}12 kcal, less than, but still close to, that observed for Al-Si order in anorthite. TEM investigation shows antiphase domains and Carlsbad twins the size of whi...
Framework silicates are the most abundant constituents of the Earth's crust and upper mantle. Feldsp...
We determined the cation distribution and ordering of Si, Al and Fe on the tetrahedral sites of a m...
Limits of solid solution in the system NaAlSi₃O₈-KAlSi₃O₈ have been studied in many ways by many ind...
Al-Si ordering in Sr-feldspar has been followed by isothermal annealing, starting from a disordered ...
Feldspars crystallized in the range SrF80An20-SrF60An40 of the join CaAl2Si2O8-SrAl2Si2O8 from gels ...
In situ high-temperature synchrotron radiation powder diffraction patterns were taken from room temp...
The system NaAlSi3O8-SrAl2Si2O8 has been studied between 1 600 °C and 1 100 °C by dry crystallizatio...
, space group: I2/c) were treated isothermally in the temperature range between 1410 and 1640ëC, in ...
Lead feldspar single crystals were annealed at T = 1050 and 1000 degrees C, starting from a disorder...
The Cl = 11 AySi order/disorder transformation in intermediate plagioclase feldspars has been experi...
Slawsonite’s (SrAl2Si2O8) structure evolutions depending on temperature (27–1000 °C) have been studi...
Domain textures related to the -I2/c displacive phase transition were observed by transmission elect...
Feldspars are rock-forming minerals that make up most of the Earth’s crust. Along the mantle geother...
In the optically untwinned microperthitic alkali feldspars from the Mt. Pélago anatexites in the Arg...
Experimental, microstructural and calorimetric evidence for the stability relations among plagioclas...
Framework silicates are the most abundant constituents of the Earth's crust and upper mantle. Feldsp...
We determined the cation distribution and ordering of Si, Al and Fe on the tetrahedral sites of a m...
Limits of solid solution in the system NaAlSi₃O₈-KAlSi₃O₈ have been studied in many ways by many ind...
Al-Si ordering in Sr-feldspar has been followed by isothermal annealing, starting from a disordered ...
Feldspars crystallized in the range SrF80An20-SrF60An40 of the join CaAl2Si2O8-SrAl2Si2O8 from gels ...
In situ high-temperature synchrotron radiation powder diffraction patterns were taken from room temp...
The system NaAlSi3O8-SrAl2Si2O8 has been studied between 1 600 °C and 1 100 °C by dry crystallizatio...
, space group: I2/c) were treated isothermally in the temperature range between 1410 and 1640ëC, in ...
Lead feldspar single crystals were annealed at T = 1050 and 1000 degrees C, starting from a disorder...
The Cl = 11 AySi order/disorder transformation in intermediate plagioclase feldspars has been experi...
Slawsonite’s (SrAl2Si2O8) structure evolutions depending on temperature (27–1000 °C) have been studi...
Domain textures related to the -I2/c displacive phase transition were observed by transmission elect...
Feldspars are rock-forming minerals that make up most of the Earth’s crust. Along the mantle geother...
In the optically untwinned microperthitic alkali feldspars from the Mt. Pélago anatexites in the Arg...
Experimental, microstructural and calorimetric evidence for the stability relations among plagioclas...
Framework silicates are the most abundant constituents of the Earth's crust and upper mantle. Feldsp...
We determined the cation distribution and ordering of Si, Al and Fe on the tetrahedral sites of a m...
Limits of solid solution in the system NaAlSi₃O₈-KAlSi₃O₈ have been studied in many ways by many ind...