REGIONAL ROCKS- half baked?
The CPC is a convenient (and dated) label for the belt of similar looking granites (plutons, batholiths) from Baja to Alaska along the Pacific Coast. On closer study, it became obvious the West Coast was a patchwork of many terranes (thus likeness was from similar process of accretion rather than origin). Geologic studies in the previous several decades had been
intrigued by our CPC.
There are two
sources of heat to bake rocks: depth and molten intruded
rocks (or more
technical). 3) Plutons (molten granite intruded at depth) also changed the rocks close to them which were either pushed aside (the contour lines at "3", north of the Ecstall pluton) or even (partially liquefied ("Mictic" below). Thus much of Accrete projects locally have dealt with how and why plutons embedded. See granites section.
It is refreshing to see even experts disagree.
Skeena rocks have been labeled differently by people who studied
the area. (Compare the three maps on this page.) So don't feel
bad if you're not sure if the rock in hand is gneiss (foliated)
or granite; or if the metamorphic is slate, phyllite or schist.
Hutchinson 1982: Geology of the Prince Rupert - Skeena Map
Area, British Columbia Need a refresher on Metamorphic rocks? Here is a good, easy, non-technical 1st year course If that's too easy, here's a UBC 2nd year course. There is a rock e.g., greenschist look-up feature on this site. Not challenging enough? Try this meta-index for Metamorphic rocks; the list of on line journals is convenient. Back to Nature index or to local schist as street art | |||||||||
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