On the geology of lower dee-side and the southern highland border

Barrow. (1912). On the geology of lower dee-side and the southern highland border. 7878(12).

Type

Journal article

Intellectual base

Primary research

Year

1912

DOI

10.1016/s0016-7878(12)80018-6

Link

https://doi.org/10.1016/s0016-7878(12)80018-6

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

Verification

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Registry ID ref:31e332ef6553 · see in the full table