Jump to content

Talk:Back-arc basin

Page contents not supported in other languages.
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by James K. Workman (talk | contribs) at 15:50, 18 November 2012 (Please give cause and effect in lay-language: new section). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

WikiProject iconVolcanoes B‑class Mid‑importance
WikiProject iconThis article is within the scope of WikiProject Volcanoes, a collaborative effort to improve the coverage of volcanoes, volcanology, igneous petrology, and related subjects on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.
BThis article has been rated as B-class on Wikipedia's content assessment scale.
MidThis article has been rated as Mid-importance on the project's importance scale.
WikiProject iconGeology B‑class High‑importance
WikiProject iconTalk:Back-arc basin is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.
BThis article has been rated as B-class on Wikipedia's content assessment scale.
HighThis article has been rated as High-importance on the project's importance scale.

Merge

Merge is self explanatory.Rolinator 10:40, 29 October 2006 (UTC)[reply]

Done :-) Vsmith 14:37, 29 October 2006 (UTC)[reply]

Please give cause and effect in lay-language

I'm an educated person of above-average intelligence, but I couldn't see clearly the cause of back-arc basins. They seem to be a trench formed by sea-floor spreading near a major subduction zone. But I don't see the cause and effect. It seems to me that the opening section could explain this for lay-people, with details in geologic jargon in following sections.JWorkman 15:50, 18 November 2012 (UTC)