Tectonic contraction across Los Angeles after removal of groundwater pumping effects

Gerald W. Bawden (), Wayne Thatcher, Ross S. Stein, Ken W. Hudnut and Gilles Peltzer
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Gerald W. Bawden: United States Geological Survey
Wayne Thatcher: United States Geological Survey
Ross S. Stein: United States Geological Survey
Ken W. Hudnut: United States Geological Survey
Gilles Peltzer: University of California

Nature, 2001, vol. 412, issue 6849, 812-815

Abstract: Abstract After the 1987 Whittier Narrows1 and 1994 Northridge2 earthquakes revealed that blind thrust faults represent a significant threat to metropolitan Los Angeles3, a network of 250 continuously recording global positioning system (GPS) stations4,5 was deployed to monitor displacements associated with deep slip on both blind and surface faults. Here we augment this GPS data with interferometric synthetic aperture radar imagery to take into account the deformation associated with groundwater pumping and strike-slip faulting. After removing these non-tectonic signals, we are left with 4.4 mm yr-1 of uniaxial contraction across the Los Angeles basin, oriented N 36° E (perpendicular to the major strike-slip faults in the area). This indicates that the contraction is primarily accommodated on thrust faults6 rather than on the northeast-trending strike–slip faults. We have found that widespread groundwater and oil pumping obscures and in some cases mimics the tectonic signals expected from the blind thrust faults. In the 40-km-long Santa Ana basin, groundwater withdrawal and re-injection produces 12 mm yr-1 of long-term subsidence, accompanied by an unprecedented seasonal oscillation of 55 mm in the vertical direction and 7 mm horizontally.

Date: 2001
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DOI: 10.1038/35090558

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