Showing 1 - 20 results of 82 for search '"seafloor spreading"', query time: 0.11s Refine Results
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    Ignition of the southern Atlantic seafloor spreading machine without hot-mantle booster by Daniel Sauter, Gianreto Manatschal, Nick Kusznir, Charles Masquelet, Philippe Werner, Marc Ulrich, Paul Bellingham, Dieter Franke, Julia Autin

    Published 2023-01-01
    “…Here we investigate the magma budget alongside the South Atlantic margins, at the onset of seafloor spreading, using high-quality seismic reflection profiles to accurately estimate the oceanic crustal thickness. …”
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    Seismic anisotropy indicates organised melt beneath the Mid-Atlantic Ridge aids seafloor spreading by Kendall, J, Schlaphorst, D, Rychert, C, Harmon, N, Agius, M, Tharimena, S

    Published 2023
    “…Skip Nav Destination RESEARCH ARTICLE| AUGUST 04, 2023 Seismic anisotropy indicates organized melt beneath the Mid-Atlantic Ridge aids seafloor spreading J.M. Kendall; D. Schlaphorst; C.A. Rychert; N. …”
    Journal article
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    Timing of Seafloor Spreading Cessation at the Macquarie Ridge Complex (SW Pacific) and Implications for Upper Mantle Heterogeneity by Qiang Jiang, Renaud E. Merle, Fred Jourdan, Hugo K.H. Olierook, Martin J. Whitehouse, Katy A. Evans, Xuan‐Ce Wang, Chris E. Conway, Helen C. Bostock, Richard J. Wysoczanski

    Published 2021-01-01
    “…Abstract The Macquarie Ridge Complex (MRC) on the Australia‐Pacific plate boundary south of New Zealand is an extinct mid‐ocean ridge that has experienced a complex tectonic history and produced highly heterogeneous mid‐ocean ridge basalts (MORBs). When and how seafloor spreading ceased along the proto‐Macquarie mid‐ocean ridge remain elusive, and it is unclear how the mantle source of MORBs is affected by the gradual cessation of seafloor spreading at mid‐ocean ridges. …”
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    Lithospheric Structure and Extensional Style of the Red Sea Rift Segments by Kuruvamana Satheeshbabu Sreenidhi, Munukutla Radhakrishna, Peter G. Betts

    Published 2023-10-01
    “…These are: (i) southernmost Red Sea and Danakil having regionally weak and stretched lithosphere, (ii) southern Red Sea with fully developed seafloor spreading and asymmetric lithospheric architecture, (iii) central Red Sea having discontinuous magma accretion with newly formed seafloor spreading, and (iv) northern Red sea with a stronger lithosphere and limited stretching revealing a stage of continental rifting. …”
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