Partial melting and magma formation
Rock can begin melting without every component entering the liquid.
Key knowledge
Rock can begin melting without every component entering the liquid. Melt composition depends on source mineralogy, pressure, temperature and volatile conditions. Decompression, heat addition and volatile-induced lowering of the solidus provide different routes to melting; extracted melt can differ chemically from its source.
Conditions and scope
- A multi-component phase relation is not equivalent to independently melting pure minerals in sequence.
- Melting degree, equilibrium and extraction history must be specified.
Sources · 1
References
Sources retain their recorded scope. A source link alone does not establish verification of every statement.
Evidence and review
Read partial-melting and pressure/volatile/temperature routes; retained multi-component qualification beyond the teaching analogy.
2026-10-10 · Independent AI editorial review: All36 Life-authored Earth compact statements/conditions/displayed equations and all81 origin semantic links read; all36 author exact-source matrix rows and exclusions assessed. All18 inherited Earth compact records read for combined inventory. Targeted independent actual primary sections listed below; not every source body or proof independently reread. AI editorial reference review, not human certification/field proficiency or whole-field completion. Receipt: earth-life-independent-content-review.1.
Entry details
Permanent link to this entry ↗- Record identity
- uni-earth-partial-melting
- Revision
- core.1
- Structured reference record
- University core expansion