Direct measurement of fault rupture using seismic dense arrays : Method and application to the Alpine Fault, New Zealand and SMART-1, Taiwan data (2004)
Type of ContentTheses / Dissertations
Thesis DisciplineCivil Engineering
Degree NameDoctor of Philosophy
PublisherUniversity of Canterbury. Civil Engineering
AuthorsFrancois-Holden, Carolineshow all
A dense network of strong motion seismometers is being developed for the central South Island of New Zealand in order to investigate the complexities of the upper crustal rupture process and propagation of major seismogenic sources such as the Alpine Fault and strands of the Marlborough Fault System defining the South Island sector of the Australia-Pacific plate boundary zone. Dense array analysis allows one to measure directly fault rupture parameters such as the rupture direction, velocity, and fault rupture area. This study develops and applies dense array analysis to determine an optimal array for the Alpine Fault region. The dense array analysis is based on the frequency-analysis MUSIC method (Multiple Signal Characterization) developed by Goldstein and Archuleta (1991a&b). MUSIC was chosen for its ability to resolve seismic signals with low signal-to-noise ratios. Careful programming, thorough data pre-processing and an innovative optimal time window determination were essential in obtaining reliable results. The proposed network is designed as a dense array comprising approximately 12 accelerographs utilising the University of Canterbury CUSP instrument. It will be deployed immediately to the East of the East-dipping Alpine Fault in the central West Coast region of the South Island, with coverage extending across to the Alpine-Hope Fault junction. The search for an optimal network for the region is dependant not only on finding an optimal array configuration but also and more significantly on optimal site locations, which because of the mountainous terrain provides a severe limitation. In order to assess the efficiency of dense array analysis, synthetic data were generated for known rupture scenarios. The synthetic strong-motion records were computed using an empirical Green's function synthetic seismogram program EMPSYN (Hutchings, 1987). Comparison of computed rupture parameters with synthetic known inputs has proven that the technique is efficient in reproducing fault rupture scenarios. The analysis provides rupture velocities and directions consistent with input values. These results are an important outcome to validate dense array analysis performed on real data sets. However, dense array analysis could reveal no sign of an asperity in the synthetic scenario. The method is applied to a real dataset recorded at the dense SMART-1 array in Taiwan. Important rupture parameters such as the direction of propagation, velocity and rupture area were successfully measured. In addition, an interesting feature of the real rupture is also identified. The fault rupture initiates at a super-shear velocity and eventually slows to a "cruising" velocity closer to the shear-wave velocities. This result supports the emerging theory that a fault rupture velocity is not constant.