Partial Melting of a Fertile Mantle Peridotite at High Pressures: An Experimental Study Using Aggregates of Diamond

2013 ◽  
pp. 109-122 ◽  
Author(s):  
Ikuo Kushiro
Keyword(s):  
Experimental Study ◽  
Partial Melting ◽  
High Pressures ◽  
Mantle Peridotite

EXPERIMENTAL STUDY OF THE SOLUBILITY OF URANINITE IN GRANITIC MELTS AND FLUID SOLUTIONS AT HIGH PRESSURES AND TEMPERATURES

1987 ◽  
Vol 29 (8) ◽  
pp. 997-1004 ◽  
Author(s):  
V. A. Zharikov ◽  
I. P. Ivanov ◽  
B. I. Omel'yanenko ◽  
A. F. Red'kin ◽  
S. V. Yudintsev
Keyword(s):  
Experimental Study ◽  
High Pressures ◽  
High Pressures And Temperatures

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

Experimental study on flame spread along fuel cylinders in high pressures

2019 ◽  
Vol 43 (8) ◽  
pp. 1022-1030
Author(s):  
Yanli Zhao ◽  
Jian Chen ◽  
Youjie Sheng ◽  
Xiao Chen ◽  
Shouxiang Lu
Keyword(s):  
Experimental Study ◽  
Flame Spread ◽  
High Pressures

Experimental study of isobaric specific heat of higher alcohols at high pressures

1986 ◽  
Vol 51 (6) ◽  
pp. 1459-1464 ◽  
Author(s):  
Ya. M. Naziev ◽  
M. M. Bashirov ◽  
Yu. A. Badalov
Keyword(s):  
Experimental Study ◽  
Specific Heat ◽  
High Pressures ◽  
Higher Alcohols ◽  
Isobaric Specific Heat

Geochemical evidence for the emplacement of the Whin Sill complex of northern England

1985 ◽  
Vol 122 (4) ◽  
pp. 389-396 ◽  
Author(s):  
R. S. Thorpe ◽  
R. Macdonald
Keyword(s):  
Trace Elements ◽  
Trace Element ◽  
Partial Melting ◽  
Sedimentary Rocks ◽  
Crustal Contamination ◽  
Mantle Peridotite ◽  
Chemical Characteristics ◽  
Heterogeneous Mantle ◽  
Magma Pulses ◽  
Significant Chemical

AbstractThe Whin Sill comprises a major quartz tholeiite sill of late Carboniferous age underlying an area of c. 5000 km2 and with a volume of c. 200 km3, associated with contemporaneous dykes emplaced within Carboniferous sedimentary rocks in northeast England. New trace element analyses of chilled margins, sill interiors and dykes indicate that the Whin Sill complex magmas show significant chemical variations in terms of the relatively stable trace elements Th, Ce, Y, Zr, Nb and Ni. These data indicate that the complex was fed by a large number of compositionally distinct magma pulses, and that certain of the dykes may have formed feeder channels for the sill. The chemical characteristics of the sill and dyke samples are consistent with derivation by extensive polybaric fractional crystallization of olivine tholeiite magma derived by partial melting of compositionally heterogeneous mantle peridotite and/or crustal contamination of mantle-derived magmas.

Deformation-induced decomposition of enstatite in mantle peridotite and its role in partial melting and chromite ore formation

2017 ◽  
Vol 476 (1) ◽  
pp. 1058-1061 ◽  
Author(s):  
D. E. Saveliev ◽  
V. N. Puchkov ◽  
S. N. Sergeev ◽  
I. I. Misabirov
Keyword(s):  
Partial Melting ◽  
Mantle Peridotite ◽  
Ore Formation ◽  
Chromite Ore ◽  
Induced Decomposition
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