| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699692 | Chemical Geology | 2011 | 14 Pages |
Abstract
⺠Crystal textures and compositions change as a function of cooling rate from dike core-to-rim. ⺠Crystals do not re-equilibrate with the melt at the dike rim. ⺠The composition of crystals experiencing rapid cooling rates suggests high-temperature formation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Silvio Mollo, Gabriele Lanzafame, Matteo Masotta, Gianluca Iezzi, Carmelo Ferlito, Piergiorgio Scarlato,