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- W2892428846 abstract "This chapter considers large oceanic intraplate earthquakes well removed from clearly defined plate boundaries and their relationship to fracture zones and plate stresses. Most earthquakes of this type involve predominantly strike-slip faulting, and events with magnitudes ≥ 7.8 have been observed in the Atlantic, Pacific, Antarctic, and Indo-Australian plates. Intensive intraplate strike-slip and reverse faulting activity is observed in the diffuse Indo-Australian deformation zone, produced by evolving plate boundary stress conditions. In some cases, the strike-slip faulting appears to be located directly on fracture zone structures, but in other cases, including the great 2012 Indo-Australian magnitude 8.6 earthquake, faulting occurs on faults offset or at high angles to fracture zones, sometimes on structures that parallel former ridge segments. The intraplate activity in the deformation zone mostly appears to be constrained to above the 600°C isotherm at depths less than 40–50 km, however, slip inversions for several large events suggest deeper rupture to near 60 km that may extend across the entire lithosphere." @default.
- W2892428846 created "2018-10-05" @default.
- W2892428846 creator A5055979975 @default.
- W2892428846 date "2019-01-01" @default.
- W2892428846 modified "2023-10-06" @default.
- W2892428846 title "Reactivation of Oceanic Fracture Zones in Large Intraplate Earthquakes?" @default.
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- W2892428846 doi "https://doi.org/10.1016/b978-0-12-812064-4.00004-9" @default.
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