PETROGRAPHY, AGE AND PROVENANCE OF MAFIC DIKES, WESTERN MAINE
The basaltic dikes range in thickness from < 1m to 4m across and have well developed chilled margins. They are mostly aphyric in texture, although some of the larger dikes are coarser grained in their centers and should be termed diabase. Some porphyritic examples are also observed containing small cm-sized, randomly oriented plagioclase lathes. In thin section many of the dikes may contain titanaugite although this needs to be confirmed with microprobe data. Another set of dikes that cross cut the basalt/diabase dikes are trachybasalts compositionally and contain glomerocrysts composed of plagioclase and aergerine (?). These dikes are most likely related to nearby alkaline stocks.
Geochemically the basaltic dikes are mostly alkaline in composition, plot in the “within plate” alkali basalt field on trace element discrimination diagrams and display the high TiO2 levels observed in dikes of the CNE suite. However, there are notable exceptions to this, with some of the dikes not conforming to this pattern. Indeed new preliminary 40Ar/39Ar integrated ages of 228.4± 4.9Ma and 197.0±1Ma may suggest two pulses of dike emplacement. Therefore, while most of the basaltic activity can be related to the older CNE suite there may be some representatives of CAMP magmatism in this part of northern New England.