Deformation structure and exhumation process of the Laojunshan gneiss dome in southeastern Yunnan of China

2021 ◽  
Vol 64 (12) ◽  
pp. 2190-2216
Author(s):  
Zhong Liu ◽  
Shuyun Cao ◽  
Yanlong Dong ◽  
Wei Li ◽  
Xuemei Cheng ◽  
...  
Keyword(s):  
Deformation Structure ◽  
Gneiss Dome

Investigation of shock-wave deformation history from recovered structure

1986 ◽  
Vol 44 ◽  
pp. 434-435
Author(s):  
M.A. Mogilevsky ◽  
L.S. Bushnev
Keyword(s):  
Shock Wave ◽  
Plastic Deformation ◽  
Dislocation Density ◽  
Shock Waves ◽  
Shock Front ◽  
Single Crystals ◽  
Residual Deformation ◽  
Deformation Structure ◽  
Deformation History ◽  
Deformation Velocity

Single crystals of Al were loaded by 15 to 40 GPa shock waves at 77 K with a pulse duration of 1.0 to 0.5 μs and a residual deformation of ∼1%. The analysis of deformation structure peculiarities allows the deformation history to be re-established.After a 20 to 40 GPa loading the dislocation density in the recovered samples was about 1010 cm-2. By measuring the thickness of the 40 GPa shock front in Al, a plastic deformation velocity of 1.07 x 108 s-1 is obtained, from where the moving dislocation density at the front is 7 x 1010 cm-2. A very small part of dislocations moves during the whole time of compression, i.e. a total dislocation density at the front must be in excess of this value by one or two orders. Consequently, due to extremely high stresses, at the front there exists a very unstable structure which is rearranged later with a noticeable decrease in dislocation density.

Age of emplacement of the Okanogan gneiss dome, north-central Washington

1976 ◽  
Vol 87 (9) ◽  
pp. 1217 ◽  
Author(s):  
K. F. FOX ◽  
C. D. RINEHART ◽  
J. C. ENGELS ◽  
T. W. STERN
Keyword(s):  
Gneiss Dome ◽  
North Central

Multistage magmatism recorded in a single gneiss dome: Insights from the Lhagoi Kangri leucogranites, Himalayan orogen

Lithos ◽  
2021 ◽  
pp. 106222
Author(s):  
Shao-Xiong He ◽  
Xiao-Chi Liu ◽  
Lei Yang ◽  
Jia-Min Wang ◽  
Fang-Yang Hu ◽  
...  
Keyword(s):  
Gneiss Dome ◽  
Himalayan Orogen

Syntectonic 1.46 Ga magmatism and rapid cooling of a gneiss dome in the southern Mazatzal Province: Burro Mountains, New Mexico

2011 ◽  
Vol 123 (9-10) ◽  
pp. 1720-1744 ◽  
Author(s):  
J. M. Amato ◽  
M. T. Heizler ◽  
A. O. Boullion ◽  
A. E. Sanders ◽  
J. Toro ◽  
...  
Keyword(s):  
New Mexico ◽  
Gneiss Dome ◽  
Rapid Cooling

scholarly journals Cretaceous oblique extensional deformation and magma accumulation in the Fosdick Mountains migmatite-cored gneiss dome, West Antarctica

Tectonics ◽  
2010 ◽  
Vol 29 (4) ◽  
pp. n/a-n/a ◽  
Author(s):  
R. R. McFadden ◽  
C. S. Siddoway ◽  
C. Teyssier ◽  
C. M. Fanning
Keyword(s):  
West Antarctica ◽  
Gneiss Dome ◽  
Extensional Deformation

A Carbon Black Structure-Concentration Equivalence Principle. Application to Stress-Strain Relationships of Filled Rubbers

1971 ◽  
Vol 44 (1) ◽  
pp. 199-213 ◽  
Author(s):  
Gerard Kraus
Keyword(s):  
Carbon Black ◽  
Primary Structure ◽  
Equivalence Principle ◽  
Chemical Activity ◽  
Cross Linking ◽  
Surface Chemical ◽  
Deformation Structure ◽  
Carbon Blacks ◽  
Filled Rubbers ◽  
Dependent Factor

Abstract It is shown that various modulus values of carbon black reinforced rubber are functions of the product of the actual black loading and a structure dependent factor. The structure factor appears to be a linear function of the so-called 24M4 value of the dibutylphthalate absorption and is independent of elongation, temperature, and degree of cross-linking over the ranges covered by the data reported. An interpretation of the results is offered based on the idea of polymer occluded in the interstices of primary structure aggregates and thereby shielded from deformation. Structure-concentration equivalence can only be demonstrated with carbon blacks differing in (primary) structure alone. Deviations are observed whenever the carbon blacks compared vary significantly in specific surface area and surface chemical activity.

The Pelham gneiss dome, Massachusetts

1942 ◽  
Vol 23 (2) ◽  
pp. 343 ◽  
Author(s):  
Robert Balk
Keyword(s):  
Gneiss Dome
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