
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | July 19, 1995 |
Latest Amendment Date: | August 6, 1998 |
Award Number: | 9506504 |
Award Instrument: | Standard Grant |
Program Manager: |
Thomas O. Wright
EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | August 15, 1995 |
End Date: | January 31, 1999 (Estimated) |
Total Intended Award Amount: | $110,067.00 |
Total Awarded Amount to Date: | $110,067.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
2221 UNIVERSITY AVE SE STE 100 MINNEAPOLIS MN US 55414-3074 (612)624-5599 |
Sponsor Congressional District: |
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Primary Place of Performance: |
2221 UNIVERSITY AVE SE STE 100 MINNEAPOLIS MN US 55414-3074 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Tectonics |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Ductile shear zones in rocks commonly develop in three-dimensional arrays involving non-plane strains and possibly volume loss. The purpose of this project is to establish the pattern of strain and fabric development in ductile shear zones that form an anastomosing network in three dimensions, to understand the kinematics of deformation, and to test models of shear zone development. The shear zone to be studied developed in high-grade metagabbros of the Seve-koli nappes of the northern Swedish Caledonides. Preliminary strain analysis according to the planar band model of shear zone development indicates volume loss with increasing strain, yet available geochemical data indicate that deformation occurred under isochemical conditions. The three-dimensional strain analysis will be applied to the resolution of the volume loss paradox, and a successful result will be broadly applicable.
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