HAL (France)
open access
Aluminium drives hydrogen incorporation in pyrolitic lower mantle: Constraints from a combined FTIR-ERDA-nanoSIMS analysis
Hydrogen is present as hydroxyl (OH) defects in the crystal lattices of the nominally anhydrous minerals (NAMs) composing the Earth’s mantle. The NAMs comprising the lower mantle: bridgmanite, ferropericlase, and davemaoite are the three most abundant minerals on Earth, and thus their combined hydro
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
- The tetragonal-cubic transition of davemaoite: Implications for lower mantle seismic anomalies#972724
- Mid-mantle discontinuities beneath subduction zones linked to depth-dependent deformation of bridgmanite#1219597
- Melt–Rock Interaction and Metasomatism of the Lithospheric Mantle beneath the Kerguelen Plateau: Evidence from a Veined Spinel Harzburgite Xenolith#1158127
- Behavior of halogens (Cl, Br, I) in alkali-rich felsic magmas at crustal depth : an experimental approach#1146138
- Mineralogy and chemistry of basalts and secondary minerals from DSDP Site 417, Atlantic Ocean#281504
Record · ID 1434295
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