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  • Axial valley  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Gregg, Patricia M; Le Mével, H; Zhan, Yan; Dufek, Josef; Geist, Dennis; Chadwick, William W Jr (2018): Stress Triggering of the 2005 Eruption of Sierra Negra Volcano, Galápagos. Geophysical Research Letters, 45(24), 13,288-13,297, https://doi.org/10.1029/2018GL080393
    Publication Date: 2023-01-13
    Description: The following files are model data generated by COMSOL Multiphysics 5.3. Our numerical approach utilizes previously developed and benchmarked, thermomechanical and fluid-structure interaction FEM models. COMSOL Multiphysics 5.3a calculates the stress, strain, and temperature variations due to a viscous magma flowing from a deeper source into an existing, magma-filled reservoir. Model rheology implantations include: non-Temperature-dependent, Temperature-dependent, and Temperature-dependent with pre-existing weakness. Model outputs includes: Time, vertical deformation, optimized flux, change in overpressure, maximum tensile stress, and temperature.
    Keywords: File format; File name; File size; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 12 (2013): 1609–1625, doi:10.1002/ggge.20110.
    Description: We combine high-resolution bathymetry acquired using the Autonomous Underwater Vehicle ABE with digital seafloor imagery collected using the remotely operated vehicle ROPOS across the axial valley of the Southern Explorer Ridge (SER) to infer the recent volcanic and tectonic processes. The SER is an intermediate spreading ridge located in the northeast Pacific. It hosts the Magic Mountain hydrothermal vent. We reconstruct the unfaulted seafloor terrain at SER based on calculations of the vertical displacement field and fault parameters. The vertical changes between the initial and the restored topographies reflect the integrated effects of volcanism and tectonism on relief-forming processes over the last 11,000–14,000 years. The restored topography indicates that the axial morphology evolved from a smooth constructional dome 〉500 m in diameter, to a fault-bounded graben, ~500 m wide and 30–70 m deep. This evolution has been accompanied by changes in eruptive rate, with deposition of voluminous lobate and sheet flows when the SER had a domed morphology, and limited-extent low-effusion rate pillow eruptions during graben development. Most of the faults shaping the present axial valley postdate the construction of the dome. Our study supports a model of cyclic volcanism at the SER with periods of effusive eruptions flooding the axial rift, centered on the broad plateau at the summit of the ridge, followed by a decrease in eruptive activity and a subsequent dominance of tectonic processes, with minor low-effusion rate eruptions confined to the axial graben. The asymmetric shape of the axial graben supports an increasing role of extensional processes, with a component of simple shear in the spreading processes.
    Description: Funding for the 2002 Submarine Ring of Fire expedition was from the NOAA Ocean Exploration Program and NOAA’s Pacific Marine Environmental Laboratory. This work was supported by a Woods Hole Oceanographic Institution Post-doctoral Scholarship, CNRS and Université de Bretagne Occidentale, France.
    Description: 2013-11-29
    Keywords: Mid-ocean ridge ; Lava flow ; Spreading ; Axial valley ; Explorer ridge ; Dike ; Cyclic
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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