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Statements

Subject Item
dbr:Bahr_el_Arab_rift
rdf:type
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Rift del Bahr al-Arab Рифт Бахр-ель-Араб Bahr el Arab Rift Bahr el Arab rift
rdfs:comment
Bahr el Arab Rift ist eine geologische Großstruktur im Südwesten des Sudan. Il rift del Bahr al-Arab è un'importante formazione geologica del Sudan sudoccidentale. Il rift del Bahr al-Arab (fiume degli Arabi) è costituito dalla depressione (graben) di Baggara, tra la Repubblica Centrafricana e le Montagne di Nuba a est, e la vasta regione paludosa del Sudd a meridione. Il rift termina a nord con i depositi del Mesozoico a sud del . La fossa di mostra una estesa fagliazione che aumenta andando verso sud e raggiunge una profondità di 5 km presso i campi petroliferi Unity oil field e di 11 km a sud dei campi petroliferi di Bentiu. The Bahr el Arab rift is a major geological feature in the southwest Sudan. The Bahr el Arab rift is made up of the Baggara graben, between the Central African Republic and the Nuba Mountains to the east, and the Sudd graben further south. It terminates to the north on the faulted Mesozoic deposits south of the Darfur Dome.The Babanusa trough has extensive faulting, increasing towards the south, reaching a depth of 5 km at the Unity oil field and 11 km south of the Bentiu oil fields. Рифт Бахр-ель-Араб — провідна геологічна зона південно-західного Судану.
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dbo:abstract
Рифт Бахр-ель-Араб — провідна геологічна зона південно-західного Судану. The Bahr el Arab rift is a major geological feature in the southwest Sudan. The Bahr el Arab rift is made up of the Baggara graben, between the Central African Republic and the Nuba Mountains to the east, and the Sudd graben further south. It terminates to the north on the faulted Mesozoic deposits south of the Darfur Dome.The Babanusa trough has extensive faulting, increasing towards the south, reaching a depth of 5 km at the Unity oil field and 11 km south of the Bentiu oil fields. Bahr el Arab Rift ist eine geologische Großstruktur im Südwesten des Sudan. Il rift del Bahr al-Arab è un'importante formazione geologica del Sudan sudoccidentale. Il rift del Bahr al-Arab (fiume degli Arabi) è costituito dalla depressione (graben) di Baggara, tra la Repubblica Centrafricana e le Montagne di Nuba a est, e la vasta regione paludosa del Sudd a meridione. Il rift termina a nord con i depositi del Mesozoico a sud del . La fossa di mostra una estesa fagliazione che aumenta andando verso sud e raggiunge una profondità di 5 km presso i campi petroliferi Unity oil field e di 11 km a sud dei campi petroliferi di Bentiu.
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wikipedia-en:Bahr_el_Arab_rift