Talk:Growth fault

A fact from Growth fault appeared on Wikipedia's Main Page in the Did you know column on 24 November 2013. The text of the entry was as follows:

Did you know... that growth faults form in the sediments parallel to the margin of a continent and can form a reservoir for oil?

A record of the entry may be seen at Wikipedia:Did you know archive/2013/November. The nomination discussion and review may be seen at Template:Did you know nominations/Growth fault.

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	This article was accepted on 16 November 2013 by reviewer Huon (talk · contribs).

Geology Mid‑importance

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Mid	This article has been rated as Mid-importance on the project's importance scale.

Your page was extremely informative and had nice figures. I only have a few suggestions:

My biggest suggestion is that you have someone proofread your page; you have grammatical errors throughout.
There are a number of run-on sentences that need to be broken up into separate sentences, or they would greatly benefit from the use of commas.
Can you include a link to the "rift-drift stage" in the Driving force section?

Melissausburn (talk) 01:16, 19 November 2013 (UTC)Reply

Emad

I love your original figures, very nice detail.
I saw a few things that might help you out, aside from the grammatical mistakes:
Add more linked words. This page is very informative and most readers might need to educate themselves further to understand it.
You reference Figure 1 in the intro, but don't have FIG.1 in the text.
More images would help break up the density of the material of the page.
List actual locations were they are found.
In the driving force section, you mention "viscous", this is such a key word in plate tectonics in general, I think you should have a link or an explanation in the text.
Dynamics section needs to be moved up at least one section, if not right under the introduction. This would give a better flow to the page.
Last section "importance" may-be say why oil and gas seek out that grain size and layer thickness.

Sara8s001 (talk) 02:15, 19 November 2013 (UTC)Reply

This page was redesigned at the edge.