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We analyse the orientation of the stress field in the southern Hikurangi subduction zone, New Zealand, using focal mechanism inversions, S-wave splitting fast directions, and gravitational stresses. Here, the oceanic Pacific plate is being obliquely subducted beneath the continental Australian Plate in the New Zealand plate boundary zone.
As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work.