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- W2022787535 abstract "[1] We test the possibility of mechanical interaction between eight central volcanoes in the central part of the active Iceland rift zone. The average distance between the volcanoes is 30 km; all are thought to have shallow magma chambers, and many contain collapse calderas. We analyzed many finite-element models with the volcanoes subject to a tensile stress of 5 MPa (equal to the maximum in situ tensile strength of the crust) in a direction parallel to the spreading vector, N105°E. The results show zones between many nearby volcanoes where the tensile stresses exceed the in situ tensile strength of the crust. The results indicate that mechanical interaction between volcanoes in a pair, such as simultaneous dike emplacement, seismogenic faulting, and deformation, may be common in this part of Iceland, in agreement with observations." @default.
- W2022787535 created "2016-06-24" @default.
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- W2022787535 date "2007-05-26" @default.
- W2022787535 modified "2023-10-16" @default.
- W2022787535 title "Mechanical interaction between active volcanoes in Iceland" @default.
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- W2022787535 doi "https://doi.org/10.1029/2007gl029873" @default.
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