Dykes vs sills (NERC grant NE/J021520/1)
Description
Data on the average aspect ratio (length/width) and average length of plagioclase grains in dykes and sills, used to demonstrate that the solidification regime is a function of the orientation of tabular intrusions. The data are written up, with publication expected in Journal of Petrology.
Resources
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Description |
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http://www.bgs.ac.uk/services/ngdc/accessions/index.html#item105129 |
Tags
- nerc_ddc
- dykes
- dolerite
- convection
- plagioclase
- ngdc-deposited-data
- sills