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Deformed agglomerates near Tintagel, North Cornwall

1971; Cambridge University Press; Volume: 108; Issue: 5 Linguagem: Inglês

10.1017/s0016756800056417

1469-5081

David Hobson,

Groundwater and Isotope Geochemistry

Summary It is shown that fragments in agglomerates, which occur in chlorite schists near Tintagel, may have been both flattened and constricted. Flattening was probably associated with formation of the schistosity, and constriction with later boudinage.