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Tectonic tremor and deep slow slip on the Alpine Fault
Author(s) -
Wech A. G.,
Boese C. M.,
Stern T. A.,
Townend J.
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2012gl051751
Subject(s) - geology , seismology , subduction , crust , episodic tremor and slip , tectonics , plate tectonics , fault (geology) , strike slip tectonics , slip (aerodynamics) , transform fault , geophysics , physics , thermodynamics
Tectonic tremor is characterized by persistent, low‐frequency seismic energy seen at major plate boundaries. Although predominantly associated with subduction zones, tremor also occurs along the deep extension of the strike‐slip San Andreas Fault. Here we present the first observations of tectonic tremor along New Zealand's Alpine Fault, a major transform boundary that is late in its earthquake cycle. We report tectonic tremor that occurred on the central section of the Alpine Fault on 12 days between March 2009 and October 2011. Tremor hypocenters concentrate in the lower crust at the downdip projection of the Alpine Fault; coincide with a zone of high P‐wave attenuation (low Q p ) and bright seismic reflections; occur in the 25–45 km depth range, below the seismogenic zone; and may define the deep plate boundary structure extending through the lower crust and into the upper mantle. We infer this tremor to represent slow slip on the deep extent of the Alpine Fault in a fluid‐rich region marked by high attenuation and reflectivity. These observations provide the first indication of present‐day displacement on the lower crustal portion of the Australia–Pacific transform plate boundary.