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How have thick evaporites affected early sea-floor spreading magnetic anomalies in the Central Red Sea?

Autor: Oke I Okwokwo, Neil C Mitchell, Wen Shi, I C F Stewart, A Y Izzeldin

Publikováno v: Okwokwo, O & Mitchell, N 2022, ' How have thick evaporites affected early sea-floor spreading magnetic anomalies in the Central Red Sea? ', Geophysical Journal International, vol. 229, no. 3, pp. 1550–1566 . https://doi.org/10.1093/gji/ggac012

SUMMARYThe axial region of the Central Red Sea has been shown to be floored by oceanic crust, but this leaves the low amplitudes of off-axis magnetic anomalies to be explained. Furthermore, if seafloor spreading occurred in the late Miocene, it is un

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d3de94702f7647a04fb07f714332d97f
https://www.research.manchester.ac.uk/portal/en/publications/how-have-thick-evaporites-affected-early-seafloor-spreading-magnetic-anomalies-in-the-central-red-sea(20a6af1f-caff-4e7d-85e6-74efbbb15da1).html

Improving Constraints on Planetary Interiors With PPs Receiver Functions

Autor: William B. Banerdt, Rakshit Joshi, Benoit Tauzin, P. H. Lognonné, Quancheng Huang, Jessica C. E. Irving, Savas Ceylan, Foivos Karakostas, Domenico Giardini, V. Lekic, Do-Yeon Kim, Brigitte Knapmeyer-Endrun, Amir Khan, Mark P. Panning, Ross Maguire, Nicholas Schmerr, Mark A. Wieczorek

Publikováno v: Journal of Geophysical Research. Planets
Journal of Geophysical Research: Planets, 126 (11)
Journal of Geophysical Research. Planets, 2021, 126, pp.2553-2571. ⟨10.1029/2021JE006983⟩
Kim, D, Lekić, V, Irving, J C E, Schmerr, N, Knapmeyer-Endrun, B, Joshi, R, Panning, M P, Tauzin, B, Karakostas, F, Maguire, R, Huang, Q, Ceylan, S, Khan, A, Giardini, D, Wieczorek, M A, Lognonné, P & Banerdt, W B 2021, ' Improving Constraints on Planetary Interiors With PPs Receiver Functions ', Journal of Geophysical Research: Planets, vol. 126, no. 11, e2021JE006983 . https://doi.org/10.1029/2021JE006983

Seismological constraints obtained from receiver function (RF) analysis provide important information about the crust and mantle structure. Here, we explore the utility of the free-surface multiple of the P-wave (PP) and the corresponding conversions

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bab08015171c39698e7b0707658deb85
https://pubmed.ncbi.nlm.nih.gov/34824966

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