A few weeks ago I had the opportunity to go on a field trip to see some Neoproterozoic turbidites in the Canadian Rockies (see this post). While the detailed sedimentologic and stratigraphic work is being done on a relatively undeformed section, the mountains in this region are chock full of folded and faulted strata. I thought this one was particularly spectacular.
Okay, all you structural geology geeks ... what are we looking at? Give me some wildly comprehensive interpretations based on this one photo.
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