HAL (France)
open access
Mid-mantle discontinuities beneath subduction zones linked to depth-dependent deformation of bridgmanite
Abstract Bridgmanite, the main mineralogical phase in the Earth’s lower mantle, is intrinsically anisotropic and may therefore generate seismic anisotropy in actively-deforming regions, particularly subduction zones. The bulk of the lower mantle is widely regarded as well-mixed but recent seismic ob
Conceptio Open Archive
Analyze & explore related research in Conceptio
Connect this record directly into your research workflow or AI agent. Explore citations across open repositories, query full text, and export structured proof bundles.
This document is indexed with metadata only: full text is not available in the archive for this record. Open the official source ↗
Related documents
- Fractionated nickel isotopic compositions in the subducting slab – implications for mantle heterogeneity#347827
- Rock dredge- to sample-scale extreme petrological and chemical variability in abyssal peridotites: Extensive melt-rock reactions in the shallow oceanic mantle (Mid-Atlantic Ridge, 24.5°-25°N)#218080
- Water exchange process and bulk composition regulate slab dynamics and deep earthquakes#976250
- Melt–Rock Interaction and Metasomatism of the Lithospheric Mantle beneath the Kerguelen Plateau: Evidence from a Veined Spinel Harzburgite Xenolith#1158127
- (Table 2) The average major-element chemistry and normative mineralogy of the basaltic rock units from ODP Hole 124-770C#149699
Record · ID 1219597
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Bring this data into your agent: Connect via MCP or API · 20 free credits to start · no card required
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive