Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q12109326> ?p ?o }
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- Q12109326 subject Q6977665.
- Q12109326 subject Q7073142.
- Q12109326 abstract "The geological basement of the central and eastern regions Equatorial Guinea is composed of Precambrian rocks which form a part of the Congo craton. They include gneiss, greenstone, schist-amphibolite and granitoids. These older rocks are overlain by sedimentary rocks of Mesozoic, Neogene and Quaternary age in the west and along the coast. The islands of Pagalu and Bioko (Annobon and Fernando Poo) are of relatively recent volcanic origin, forming a part of the Cameroon Volcanic Line.".
- Q12109326 wikiPageWikiLink Q103910.
- Q12109326 wikiPageWikiLink Q103924.
- Q12109326 wikiPageWikiLink Q15315.
- Q12109326 wikiPageWikiLink Q166409.
- Q12109326 wikiPageWikiLink Q1995951.
- Q12109326 wikiPageWikiLink Q205022.
- Q12109326 wikiPageWikiLink Q2143968.
- Q12109326 wikiPageWikiLink Q26185.
- Q12109326 wikiPageWikiLink Q335239.
- Q12109326 wikiPageWikiLink Q3736616.
- Q12109326 wikiPageWikiLink Q595991.
- Q12109326 wikiPageWikiLink Q659596.
- Q12109326 wikiPageWikiLink Q6977665.
- Q12109326 wikiPageWikiLink Q7073142.
- Q12109326 wikiPageWikiLink Q8072.
- Q12109326 wikiPageWikiLink Q82480.
- Q12109326 wikiPageWikiLink Q83222.
- Q12109326 wikiPageWikiLink Q945773.
- Q12109326 wikiPageWikiLink Q983.
- Q12109326 comment "The geological basement of the central and eastern regions Equatorial Guinea is composed of Precambrian rocks which form a part of the Congo craton. They include gneiss, greenstone, schist-amphibolite and granitoids. These older rocks are overlain by sedimentary rocks of Mesozoic, Neogene and Quaternary age in the west and along the coast. The islands of Pagalu and Bioko (Annobon and Fernando Poo) are of relatively recent volcanic origin, forming a part of the Cameroon Volcanic Line.".
- Q12109326 label "Geology of Equatorial Guinea".