Award Abstract # 9219159
High Pressure Phase Equilibrium Studies Bearing on the Magmatic Evaluation of the Mantle and Crust

NSF Org: EAR
Division Of Earth Sciences
Recipient: UNIVERSITY OF TEXAS AT DALLAS
Initial Amendment Date: March 9, 1993
Latest Amendment Date: March 31, 1997
Award Number: 9219159
Award Instrument: Continuing Grant
Program Manager: David Lambert
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: April 1, 1993
End Date: March 31, 1998 (Estimated)
Total Intended Award Amount: $492,000.00
Total Awarded Amount to Date: $492,000.00
Funds Obligated to Date: FY 1993 = $114,400.00
FY 1994 = $116,800.00

FY 1995 = $119,200.00

FY 1996 = $121,600.00

FY 1997 = $20,000.00
History of Investigator:
  • Dean Presnall (Principal Investigator)
    dpresnall@ciw.edu
Recipient Sponsored Research Office: University of Texas at Dallas
800 WEST CAMPBELL RD.
RICHARDSON
TX  US  75080-3021
(972)883-2313
Sponsor Congressional District: 24
Primary Place of Performance: University of Texas at Dallas
800 WEST CAMPBELL RD.
RICHARDSON
TX  US  75080-3021
Primary Place of Performance
Congressional District:
24
Unique Entity Identifier (UEI): EJCVPNN1WFS5
Parent UEI:
NSF Program(s): Petrology and Geochemistry
Primary Program Source:  
app-0194 

app-0195 

app-0196 

app-0197 
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 157300
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This ongoing research has a long-term objective of developing a systematic body of liquidus phase equilibrium data on model chemical systems relevant to the origin and crystallization of the presumed early magma ocean and on the generation of magmas from the Earth's mantle. The proposed projects will utilize piston cylinder and multianvil techniques to determine the phase relationships that control the melting behavior of model amphibolite-kyanite-quartz eclogite at 3 GPa and the melting and crystallization behavior of model peridotite at pressures from 7 - 16 GPa. Results of these studies will directly address aspects of magma generation at subduction zones and will place additional constraints on the formation and crystallization of a presumed early magma ocean.

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