Metamorphic Phase Equilibria and Pressure-temperature-time Paths¶
Spear. (1993). Metamorphic Phase Equilibria and Pressure-temperature-time Paths.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Orogenic Belt
- Metamorphism in the deep hinterland — commonly reaching amphibolite or granulite facies, with pressure-temperature-time paths recorded in mineral assemblages
This sourceThe reference treatment of metamorphic phase equilibria and the recovery of pressure-temperature-time paths from mineral assemblages, including amphibolite- and granulite-facies conditions.
- Metamorphism in the deep hinterland — commonly reaching amphibolite or granulite facies, with pressure-temperature-time paths recorded in mineral assemblages
Verification¶
Does it exist? Not checked yet. This entry carries no identifier to resolve. It was extracted from the citation as written in the article, normalized, and deduplicated against the rest of the registry.
Does it back the claim? Not recorded. The single citation of this work carries no recorded support check.
Support is checked per citation rather than per work — the same source can be cited soundly in one article and wrongly in another. Per-citation recording began recently, so a citation with no recorded check is a gap in the record rather than evidence it went unchecked.
See how references were verified.
Registry ID ref:e5ebd6a2c6dc · see in the full table