Attenuation due to partial melting: An experimental study on a model system, using the Lab Coda Method

1993 ◽  
Vol 98 (B2) ◽  
pp. 1853-1860 ◽  
Author(s):  
L. S. Gao ◽  
J. P. Poirier ◽  
K. Aki
Keyword(s):  
Experimental Study ◽  
Partial Melting ◽  
Model System

Generation of alkaline magmas in subduction zones by partial melting of mélange diapirs—An experimental study

Geology ◽  
2018 ◽  
Vol 46 (4) ◽  
pp. 343-346 ◽  
Author(s):  
Alicia M. Cruz-Uribe ◽  
Horst R. Marschall ◽  
Glenn A. Gaetani ◽  
Véronique Le Roux
Keyword(s):  
Experimental Study ◽  
Partial Melting ◽  
Subduction Zones ◽  
Alkaline Magmas

An experimental study of the role of shear deformation on partial melting of a synthetic metapelite

2011 ◽  
Vol 503 (1-2) ◽  
pp. 92-99 ◽  
Author(s):  
Elizaveta Tumarkina ◽  
Santanu Misra ◽  
Luigi Burlini ◽  
James A.D. Connolly
Keyword(s):  
Experimental Study ◽  
Partial Melting ◽  
Shear Deformation

Experimental Study of Hormone Receptor Development in a Unicellular Model System

Pathobiology ◽  
1981 ◽  
Vol 49 (3) ◽  
pp. 173-176
Author(s):  
G. Csaba ◽  
G. Németh ◽  
P. Vargha
Keyword(s):  
Experimental Study ◽  
Hormone Receptor ◽  
Model System

Sulfide partial melting and galena–tetrahedrite intergrowth texture: An experimental study

2020 ◽  
pp. 1-10
Author(s):  
Boddepalli Govindarao ◽  
Kamal Lochan Pruseth ◽  
Biswajit Mishra
Keyword(s):  
Experimental Study ◽  
Partial Melting ◽  
Equilibrium Phase ◽  
Ore Deposits ◽  
Phase Assemblage ◽  
Silica Tube ◽  
Sulfide Ore ◽  
Potential Indicator ◽  
Sulfide Melt ◽  
Melting Experiments

Abstract Galena–tetrahedrite intergrowth textures have been observed in some quenched run products of melting experiments conducted at 500 and 600°C in the systems ZnS–PbS–FeS–Cu2S–Sb2S3 and ZnS–PbS–FeS–Cu2S–Sb2S3–As2S3, using the evacuated silica-tube method. At 600°C the intergrowth formed an interface between sulfide melt and galena, whereas at 500°C it existed as inclusions partially embedded or completely embedded within tetrahedrite. At 600°C tetrahedrite was absent in PbS-bearing experiments, instead galena and melt were a part of the equilibrium phase assemblage. From the disposition of the galena–tetrahedrite intergrowths at 500°C it is evident that droplets of galena–tetrahedrite melt coexisted with tetrahedrite or tetrahedrite + galena and gave rise to these intergrowths upon quenching. The intergrowths coexisting with galena probably represent compositions on the galena-rich liquidus in the galena–tetrahedrite binary and those coexisting with tetrahedrite represent points on the tetrahedrite-rich liquidus. A eutectic at galena:tetrahedrite = ~30:70, very close to 500°C is apparent. It is clearly indicated that galena–tetrahedrite intergrowths can be formed by sulfide partial melting, and could be used as a potential indicator of partial melting in metamorphosed sulfide ore deposits.

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