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- Q7110151 subject Q6984714.
- Q7110151 abstract "The Ouachita geosyncline was a major structural or sedimentary basin along southern North America. It is mostly covered by sedimentary rocks from the late Paleozoic and Mesozoic, but rocks of the former basin outcrop in the Llano Uplift near the Austin region, spanning Oklahoma and Arkansas, where it forms the Ouachita Mountains. The basin formed during the Paleozoic from the Ordovician through the Mississippian. The basin was involved in the Ouachita orogeny during the Pennsylvanian.".
- Q7110151 wikiPageWikiLink Q1612.
- Q7110151 wikiPageWikiLink Q1649.
- Q7110151 wikiPageWikiLink Q16559.
- Q7110151 wikiPageWikiLink Q2033447.
- Q7110151 wikiPageWikiLink Q373772.
- Q7110151 wikiPageWikiLink Q3835733.
- Q7110151 wikiPageWikiLink Q62100.
- Q7110151 wikiPageWikiLink Q6984714.
- Q7110151 wikiPageWikiLink Q7110152.
- Q7110151 wikiPageWikiLink Q744718.
- Q7110151 wikiPageWikiLink Q749565.
- Q7110151 wikiPageWikiLink Q75507.
- Q7110151 wikiPageWikiLink Q785020.
- Q7110151 wikiPageWikiLink Q82480.
- Q7110151 wikiPageWikiLink Q83222.
- Q7110151 wikiPageWikiLink Q837307.
- Q7110151 comment "The Ouachita geosyncline was a major structural or sedimentary basin along southern North America. It is mostly covered by sedimentary rocks from the late Paleozoic and Mesozoic, but rocks of the former basin outcrop in the Llano Uplift near the Austin region, spanning Oklahoma and Arkansas, where it forms the Ouachita Mountains. The basin formed during the Paleozoic from the Ordovician through the Mississippian. The basin was involved in the Ouachita orogeny during the Pennsylvanian.".
- Q7110151 label "Ouachita geosyncline".