On the geology of lower dee-side and the southern highland border¶
Barrow, G. (1912). On the geology of lower dee-side and the southern highland border. Proceedings of the Geologists' Association.
Cited by¶
1 citation across 1 artifact.
Domain-specific¶
- Metamorphism
- Barrow's zones, still called Barrovian metamorphism, turned a map of mineral occurrences into an ordered map of metamorphic grade across a mountain belt — the founding demonstration that a mapped sequence of index minerals can be read as progressive metamorphic grade, though both the thermal reading of those zones and their attribution to a regional gradient came after him
Supported in partVerified against the source
- Barrow's zones, still called Barrovian metamorphism, turned a map of mineral occurrences into an ordered map of metamorphic grade across a mountain belt — the founding demonstration that a mapped sequence of index minerals can be read as progressive metamorphic grade, though both the thermal reading of those zones and their attribution to a regional gradient came after him
Verification¶
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Registry ID ref:31e332ef6553 · see in the full table