scholarly journals Partial melting of phlogopite-bearing synthetic spinel- and garnet lherzolites

Harzburgite nodules from kimberlites can be subdivided into two groups on the basis of the CaO (0.24 compared with 0.96% by mass) and A1 2 O 3 (0.96 compared with 2.98% by mass) in their orthopyroxenes. Theoretically, the CaO and Al 2 O 3 from the high-Al orthopyroxenes can be quantitatively represented as garnet and clinopyroxene in solid solution, which would appear if the assemblages had been subjected to lower T or higher P . Some garnet lherzolites and orthopyroxene megacrysts from several S African localities exhibit textures indicative of exsolution of garnet and diopside from orthopyrozene during deformation and recrystallization and it is proposed that lherzolites with small amounts of garnet (less than 3 %) and diopside (less than 1 %) may have developed from an igneous harzburgite with high-Al orthopyroxene during subsolidus cooling and recrystallization. The simplest assumption in upper-mantle models, that garnet lherzolite is a relatively homogeneous rock capable of differentiation into a basaltic liquid and a ‘barren’ harzburgite residuum, must be modified to take into account different degrees of partial melting and subsequent recrystallization to metamorphic assemblages.


2019 ◽  
Author(s):  
Shane R. Dailey ◽  
◽  
Calvin G. Barnes ◽  
Susan E. Leib
Keyword(s):  

2020 ◽  
Author(s):  
Aleksi Rantanen ◽  
◽  
David Whipp ◽  
Jussi S. Heinonen ◽  
Lars Kaislaniemi ◽  
...  

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