The petrology and geochemistry of the Acheron intrusion
Subalkaline transitional gabbros have intruded the Cretaceous - Paleocene sediments of the Acheron Outlier. The gabbroic magma has differentiated in situ to form a laccolith and sill-like apophysis, as well as having a strong thermal effect on the sediments and especially the coals of the Broken Riv...
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| Language: | en |
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University of Canterbury. Geology
2012
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| Online Access: | http://hdl.handle.net/10092/6783 |