Hybrid flow sills: A new mode of igneous sheet intrusion
Three-dimensional (3-D) seismic mapping of the Vigra sill complex has revealed a series of shallow level lobate sills. This complex was emplaced ca. 55 Ma as part of the igneous activity associated with breakup of the northeast Atlantic margin. The complex consists of discordant sheets, some of whic...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2010
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