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LITHOEN

Geological process

Hydrothermal alteration

Chemical change of rock by hot aqueous fluid. Fluids dissolve elements at one place and precipitate them at another, which is how elements are transported and concentrated without melting anything.

How this record is known

2
Settled consensus
Cited as the accepted position of the discipline.
1
Interpretation
Reached by reasoning from evidence, or produced by a named model.

3 of 3 claims on this page cite at least one registered source. Counts describe how each statement is known, not how likely it is to be true.

What Lithoen records

Each claim states how it is known and cites its evidence.

Established0.1–10 cm

In porphyry environments wall-rock alteration is intimately linked to narrow veins, commonly 0.1 to 10 centimetres wide, which typically make up less than 1 to 5 volume percent of the mineralised rock — while the alteration they drive extends through a far larger volume.

  • precision note: The value carried is the vein width. The volume fraction, less than 1 to 5 percent, is stated in the claim; the relation between a small vein volume and a large altered volume is the point.

Evidence support: Supported by the cited evidence one source

Evidence: John 2010 Primary authority

InferredDissolution, transport and precipitation by hot aqueous fluid.

Hot aqueous fluids move elements without melting anything: they dissolve material where conditions favour solution and precipitate it where conditions do not, transporting elements between rock volumes and altering the rock they pass through.

  • method: The cited source states that metamorphism can proceed by reaction with hot mineral-rich fluids entering the rock and that new minerals form by those reactions; the transport role follows.
  • precision note: Phase 2 records the physical and chemical bridge only. Ore-forming fluid systems belong to a later phase and are not asserted here.

Evidence support: Supported by the cited evidence 2 sources, multiple sources, independence unknown

Evidence: U.S. Geological Survey n.d. Primary authority; John 2010 Primary authority

EstablishedMetasomatic change of composition, mineralogy and texture by a hot aqueous fluid.

Hydrothermal alteration is a set of metasomatic processes that change the composition, mineralogy and texture of a rock: alkali metasomatism, hydrolytic or acidic reactions, oxidation-reduction reactions including sulfidation, solubility-induced precipitation such as quartz deposition, and hydration and carbonation reactions in which water or carbonate is added.

  • precision note: Defined here in the context of porphyry copper systems by the source, but the processes named are general to hydrothermal alteration and are recorded as such.

Evidence support: Supported by the cited evidence 2 sources, multiple sources, independence unknown

Evidence: John 2010 Primary authority; U.S. Geological Survey n.d. Primary authority

In the knowledge graph

Record last updated 2026-09-06. Corrections follow the published corrections policy; superseded claims are retained, never silently edited.