U-series isotopic disequilibrium produced during experimental melting of granitic crust: Implications for shallow-level assimilation and pluton remobilisation

2006 ◽  
Vol 70 (18) ◽  
pp. A326 ◽  
Author(s):  
K. Knesel ◽  
S. Turner ◽  
J.P. Davidson
Keyword(s):  
Shallow Level ◽  
Isotopic Disequilibrium ◽  
Experimental Melting

STRUCTURES RELATED TO THE EMPLACEMENT OF SHALLOW-LEVEL INTRUSIONS: A TEMPORAL ORGANIZATION

2018 ◽  
Author(s):  
David S. Westerman ◽  
◽  
Sergio Rocchi ◽  
Christoph Breitkreuz ◽  
Carl T. Stevenson
Keyword(s):  
Temporal Organization ◽  
Shallow Level

Shallow-level centers in semiconductors – 2000

2001 ◽  
Vol 302-303 ◽  
pp. 425-434 ◽  
Author(s):  
C.A.J. Ammerlaan
Keyword(s):  
Shallow Level

Discriminating assimilants and decoupling deep- vs. shallow-level crystal records at Mount Adams using 238U–230Th disequilibria and Os isotopes

2009 ◽  
Vol 277 (1-2) ◽  
pp. 38-49 ◽  
Author(s):  
Brian R. Jicha ◽  
Clark M. Johnson ◽  
Wes Hildreth ◽  
Brian L. Beard ◽  
Garret L. Hart ◽  
...  
Keyword(s):  
Shallow Level ◽  
Os Isotopes ◽  
Mount Adams

Melting of Aromatic Compounds: Molecular Dynamics Simulations

1995 ◽  
Vol 408 ◽  
Author(s):  
P. W.-C. Kung ◽  
J. T. Books ◽  
C. M. Freeman ◽  
S. M. Levine ◽  
B. Vessali ◽  
...  
Keyword(s):  
Molecular Dynamics ◽  
Molecular Crystal ◽  
Constant Pressure ◽  
Molecular Crystals ◽  
Melting Transition ◽  
Melting Temperatures ◽  
Molecular Dynamics Calculations ◽  
Dynamics Simulations ◽  
Experimental Melting Point ◽  
Experimental Melting

AbstractWe have used constant pressure molecular dynamics calculations to explore the behavior at various temperatures of two molecular crystals: benzene and a brominated phenyl compound. We observed a melting transition by heating the crystals from a low temperature. In the case of benzene, we performed one heating run of about 1 ns and obtained agreement with the experimental melting point to within some 8%. We have also simulated the melting of a more complex molecular crystal that contains bromine and phenyl groups. We performed four heating runs, with different rates of heating. For total simulation times of about 100, 220, 770, and 1 I50ps, the heating runs predicted melting temperatures that differed from the experimental melting temperature by 53%, 33%, 25%, and 9% respectively.

Kinetically limited isotope exchange in a shallow level normal fault, Mineral Mountains, Utah

1996 ◽  
Vol 101 (B1) ◽  
pp. 673-685 ◽  
Author(s):  
D. E. Barnett ◽  
J. R. Bowman ◽  
C. Bromley ◽  
C. Cady
Keyword(s):  
Isotope Exchange ◽  
Normal Fault ◽  
Shallow Level

Bond length determination for transition atoms by shallow level EELFS

1996 ◽  
Vol 352-354 ◽  
pp. 32-35 ◽  
Author(s):  
R.V. Vedrinskii ◽  
A.I. Taranukhina ◽  
L.A. Bugaev ◽  
V.L. Kraizman ◽  
A.V. Morozov ◽  
...  
Keyword(s):  
Bond Length ◽  
Shallow Level ◽  
Length Determination
Sign in / Sign up

Export Citation Format

Share Document