scholarly journals Equation of state in the generalized density scaling regime studied from ambient to ultra-high pressure conditions

2014 ◽  
Vol 140 (4) ◽  
pp. 044502 ◽  
Author(s):  
A. Grzybowski ◽  
K. Koperwas ◽  
M. Paluch
Keyword(s):  
High Pressure ◽  
Equation Of State ◽  
Ultra High Pressure

scholarly journals Characterization of GEKKO/HIPER-Driven Shock Waves for Equation-of-State Experiments in Ultra-High-Pressure Regime

2004 ◽  
Vol 80 (6) ◽  
pp. 486-491 ◽  
Author(s):  
Norimasa OZAKI ◽  
Kazuo A. TANAKA ◽  
Takatoshi ONO ◽  
Kikuo TAKAMATSU ◽  
Keiji NAGAI ◽  
...  
Keyword(s):  
High Pressure ◽  
Equation Of State ◽  
Shock Waves ◽  
Ultra High Pressure ◽  
Pressure Regime

Band-reordering effects in the ultra-high-pressure equation of state of lithium

1985 ◽  
Vol 15 (11) ◽  
pp. L247-L251 ◽  
Author(s):  
W G Zittel ◽  
J Meyer-ter-Vehn ◽  
J C Boettger ◽  
S B Trickey
Keyword(s):  
High Pressure ◽  
Equation Of State ◽  
Pressure Equation ◽  
Ultra High Pressure

Equation of state of rhenium and application for ultra high pressure calibration

2014 ◽  
Vol 115 (4) ◽  
pp. 043511 ◽  
Author(s):  
Simone Anzellini ◽  
Agnès Dewaele ◽  
Florent Occelli ◽  
Paul Loubeyre ◽  
Mohamed Mezouar
Keyword(s):  
High Pressure ◽  
Equation Of State ◽  
Ultra High Pressure ◽  
Pressure Calibration

scholarly journals Trans-lithospheric diapirism explains the presence of ultra-high pressure rocks in the European Variscides

2021 ◽  
Vol 2 (1) ◽  
Author(s):  
Petra Maierová ◽  
Karel Schulmann ◽  
Pavla Štípská ◽  
Taras Gerya ◽  
Ondrej Lexa
Keyword(s):  
High Pressure ◽  
Numerical Models ◽  
Classical Concept ◽  
Plate Interface ◽  
Ultra High Pressure ◽  
Common Process ◽  
Mountain Belts ◽  
Collisional Orogens ◽  
Rock Association ◽  
European Variscides

AbstractThe classical concept of collisional orogens suggests that mountain belts form as a crustal wedge between the downgoing and overriding plates. However, this orogenic style is not compatible with the presence of (ultra-)high pressure crustal and mantle rocks far from the plate interface in the Bohemian Massif of Central Europe. Here we use a comparison between geological observations and thermo-mechanical numerical models to explain their formation. We suggest that continental crust was first deeply subducted, then flowed laterally underneath the lithosphere and eventually rose in the form of large partially molten trans-lithospheric diapirs. We further show that trans-lithospheric diapirism produces a specific rock association of (ultra-)high pressure crustal and mantle rocks and ultra-potassic magmas that alternates with the less metamorphosed rocks of the upper plate. Similar rock associations have been described in other convergent zones, both modern and ancient. We speculate that trans-lithospheric diapirism could be a common process.

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