Award Abstract # 0112058
Margins: Collaborative Research: Seismic and Geologic Study of Gulf of California Rifting and Magmatism

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF CALIFORNIA SAN DIEGO
Initial Amendment Date: September 13, 2001
Latest Amendment Date: January 15, 2003
Award Number: 0112058
Award Instrument: Standard Grant
Program Manager: Bilal U. Haq
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: April 1, 2002
End Date: March 31, 2007 (Estimated)
Total Intended Award Amount: $516,247.00
Total Awarded Amount to Date: $525,755.00
Funds Obligated to Date: FY 2001 = $516,247.00
FY 2003 = $9,508.00
History of Investigator:
  • Graham Kent (Principal Investigator)
    gkent@seismo.unr.edu
  • Alistair Harding (Co-Principal Investigator)
Recipient Sponsored Research Office: University of California-San Diego Scripps Inst of Oceanography
8622 DISCOVERY WAY # 116
LA JOLLA
CA  US  92093-1500
(858)534-1293
Sponsor Congressional District: 50
Primary Place of Performance: University of California-San Diego Scripps Inst of Oceanography
8622 DISCOVERY WAY # 116
LA JOLLA
CA  US  92093-1500
Primary Place of Performance
Congressional District:
50
Unique Entity Identifier (UEI): QJ8HMDK7MRM3
Parent UEI: QJ8HMDK7MRM3
NSF Program(s): Marine Geology and Geophysics,
OCEAN DRILLING PROGRAM
Primary Program Source: 01000102DB NSF RESEARCH & RELATED ACTIVIT
app-0103 
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 162000, 572000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Funding is provided for a seismic and structural geology experiment to delineate the geometries and patterns of crustal extension and rift magmatism along three main conjugate margins across Alarcon, Guaymas and Delfin Basins (to study the south to north seafloor-spreading to non-spreading mode) and a E-W profile along Wagner Basin (to study the low-angle detachment fault at depth). The questions to be addressed include, strain partitioning, volumetric and emplacement style of rift magmatism, along-axis differences in extension style and the influence of sedimentation on deformation. An integrated land-based and at sea study is planned for the next three years.


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