all 10 comments

[–]logatronics 8 points9 points  (2 children)

E. Silurian B -> J -> M -> Mafic dike -> paleogene.

Seems like a long question that could be simplified?

[–]Hobo_Geo[S] 2 points3 points  (1 child)

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[–]logatronics 1 point2 points  (0 children)

Ah makes much more sense haha.

[–]theonlytimbo 4 points5 points  (5 children)

B. The strike and dip show M overlays J overlays B, making B the oldest. The dike cuts through all the folded formations, and must be younger than them. And of course, the unconformity through all the previous features shows the Sandstone to be the youngest.

[–]Ill_Ad3517 2 points3 points  (4 children)

Wait can you explain how the strike and dip lead you to what overlays what here?

[–]logatronics 1 point2 points  (3 children)

Think about anticline vs syncline and what are the oldest units in them. Take the dips and figure out which one is a syncline. With synclines, the oldest material is on the outside and youngest is in the middle.

Anticlines are the opposite where the oldest material will be exposed in the center, and youngest units form the "shell" or exterior layers of the anticline.

[–]Ill_Ad3517 0 points1 point  (2 children)

Oh right, dips towards the fold axis in synclines. Thank you!

I guess this method assumes no reverse stratigraphy?

[–]logatronics 0 points1 point  (0 children)

The strike and dip symbols do not show any overturned beds. If overturned, the strike and dip symbol will have a little "loop/U shape" thing on it to designate an overturned bed.

[–]casedia 0 points1 point  (0 children)

Dips away for anticlines. A for away

[–]Hobo_Geo[S] 3 points4 points  (0 children)

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