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Recommended nomenclature of epidote-group minerals
Nomenclature, epidote-group minerals clinozoisite allanite dollaseite
2013/12/6
Epidote-group minerals are monoclinic in symmetry and have topology consistent with space group P21/m and the general formula A2M3[T2O7][TO4](O,F)(OH,O). Zoisite is an orthorhombic polymorph of clinoz...
Replacement of primary monazite by apatite-allanite-epidote coronas in an amphibolite facies granite gneiss from the eastern Alps
Replacement primary monazite apatite-allanite-epidote coronas eastern Alps
2012/3/31
Accessory monazite crystals in granites are commonly unstable during amphibolite fa-cies regional metamorphism and typically become mantled by newly formed apatite-allan-ite-epidote coronas. This dist...
Sr-bearing zoisite and epidote in ultra-high pressure (UHP) metamorphic rocks from the Su-Lu province, eastern China: An important Sr reservoir under UHP conditions
Sr-bearing zoisite epidote ultra-high pressure (UHP) metamorphic rocks Su-Lu province UHP conditions
2012/3/31
Sr-bearing zoisite and epidote are common constituents of eclogites and associated par-aschists throughout the Su-Lu ultra-high pressure (UHP) province, eastern China. The SrO content of prograde zois...
Solid solution between piemontite and androsite-(La), a new mineral of the epidote group from Andros Island, Greece
Solid solution piemontite androsite-(La epidote group Andros Island
2012/4/6
Anew member ofthe epidote group, androsite-(La), wasfound atAndrosIsland, Cyclades, Greece, as an accessory constituent of metamorphic Mn-rich rocks. Associated minerals are rhodochrosite, braunite, r...
Epidote in calc-alkaline magmas: An experimental study of stability, phase relationships, and the role of epidote in magmatic evolution
Epidote calc-alkaline magmas stability phase relationships the role of epidote magmatic evolution
2012/4/5
Experiments on tonalite and granodiorite wereperformed at conditions ranging from 2.1 to 18kbar and 550 to 850°C to establish the magmatic stability field ofepidote as a function ofP, T,and f02. Atwat...
Volume behavior of hydrous minerals at high pressure and temperature: II. Compressibilities of lawsonite, zoisite, clinozoisite, and epidote
Volume behavior of hydrous minerals high pressure and temperature Compressibilities of lawsonite zoisite clinozoisite epidote
2012/4/5
The pressure dependence ofthe lattice parameters ofnatural zoisite [Ca2A13Si3012(OH)], clinozoisite [Ca2A13Si30'2(OH)], and epidote [Ca2A12FeSi3012(OH)] as wellas synthetic lawsonite [CaAl2Si207(OH)2'...