Kenoran orogeny

Kenoran orogeny

[kə′nȯr·ən ȯ′räj·ə·nē]
(geology)
Mentioned in ?
References in periodicals archive ?
These rocks were intruded by Archean granites followed by mafic, ultramafic and lamprophyric dikes and sills, and were subsequently metamorphosed to greenschist facies and folded isoclinally during the Kenoran Orogeny.