Upper mantle discontinuities: anisotropic view on the lithosphere - asthenosphere system

0531147 - GFÚ 2021 RIV IT eng J - Journal Article
Plomerová, Jaroslava
Upper mantle discontinuities: anisotropic view on the lithosphere - asthenosphere system.
Bollettino di Geofisica teorica ed applicata. Roč. 61, č. 4 (2020), s. 375-402. ISSN 0006-6729. E-ISSN 2239-5695
R&D Projects: GA MŠMT(CZ) EF16_013/0001800
Institutional support: RVO:67985530
Keywords : Earth mantle discontinuities * lithosphere-asthenosphere boundary * fossil vs. present-day related large-scale anisotropy
OECD category: Volcanology
Impact factor: 0.581, year: 2020
Method of publishing: Open access
http://www3.inogs.it/bgta/provapage.php?id_articolo=854

This paper stems from a keynote “Inge Lehmann Lecture” during the ESC 2018 General Assembly and presents an overview of the historical development of Earth stratification and the corresponding discontinuities to a broader seismological community. The paper concentrates on the role of seismic velocity anisotropy in modelling the lithosphere-asthenosphere system and presents models of the lithosphere-asthenosphere boundary (LAB), the most significant tectonic boundary from the point of view of plate tectonics. With the use of anisotropic characteristics retrieved from both the surface and body waves, we model the LAB discontinuity as a narrow transition between fossil anisotropy within the mantle lithosphere and present-day flow-related anisotropy in the asthenosphere in different tectonic settings within continental and oceanic plates. The lower plate boundary lies in a relatively broad depth interval, from about 50 km beneath Phanerozoic basins up to about 220 km beneath Precambrian cratons and platforms. Beneath the oceanic plates, the discontinuity shallows up to ~30 km or even less. Distinct LAB depth variations at short distances occur particularly in Phanerozoic parts of continents.
Permanent Link: http://hdl.handle.net/11104/0309871