FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1508045386> ?p ?o ?g. }

• W1508045386 endingPage "149" @default.
• W1508045386 startingPage "105" @default.
• W1508045386 abstract "The Sudanese rift structures form intracontinental basins, bordered on all sides by anorogenic terrain. These basins are seen as the result of a multistructural system of rifts which appear to have been activated several times since the Palaeozoic. Improved methods of dating and extensive geophysical surveys have led to a better understanding of the mobile belts and the Basement rocks in the general environs of the basins, and of the elevated blocks and highs surrounding the sedimentary basins. Detailed mapping and extensive drilling in the sedimentary basins led to a better understanding of the Phanerozoic. The rapid rate of uplift and subsidence have assisted in the rapid accumulation and filling of the basins with unconsolidated sediments, ranging from a few hundred metres to some thousand metres. The rift structures contain sediments of several age groups, origin and mode of deposition. Some of them are as old as the Palaeozoic passing through to Mesozoic, Tertiary and Quaternary (Bahr El Arab rift and Blue Nile rift). The thickness of the Tertiary sediments exceeds 15 km in Bahr El Arab rift. Palaeozoic sediments were found to occupy NE-SW grabens. Jurassic? and Cretaceous sediments were deposited in NW-SE troughs. Tertiary sediments filled grabens that range in thicknesses up to 15 km. Highly saline ground-water bodies which coincide with hydrogeologically closed basins occupy the flowing end of each of the rift basins. These saline bodies have been interpreted as buried saline lakes, sabkhas or playas. Alternating wet and dry periods eventually filled up the basins with intercalating layers of fresh and saline layers. The filling up of the basins led to the interconnection of the hydrological regime and the development of the integrated River Nile. Rift structures in Sudan form the major ground-water basins, outside these basins ground water is found only in small quantities and is of poor quality. The rift basins also act as reservoirs for hydrocarbon accumulation; all the known oil fields of inland Sudan are located in these basins." @default.
• W1508045386 created "2016-06-24" @default.
• W1508045386 creator A5077546710 @default.
• W1508045386 date "1997-01-01" @default.
• W1508045386 modified "2023-10-04" @default.
• W1508045386 title "Chapter 6 Rift Basins of the Sudan" @default.
• W1508045386 cites W189764575 @default.
• W1508045386 cites W1965636393 @default.
• W1508045386 cites W1969510917 @default.
• W1508045386 cites W1971320400 @default.
• W1508045386 cites W1976864211 @default.
• W1508045386 cites W1977078184 @default.
• W1508045386 cites W1985766264 @default.
• W1508045386 cites W2008411693 @default.
• W1508045386 cites W2011189006 @default.
• W1508045386 cites W2013978370 @default.
• W1508045386 cites W2016892851 @default.
• W1508045386 cites W2017626528 @default.
• W1508045386 cites W2019451339 @default.
• W1508045386 cites W2019788090 @default.
• W1508045386 cites W2022831871 @default.
• W1508045386 cites W2029684907 @default.
• W1508045386 cites W2040389042 @default.
• W1508045386 cites W2042080396 @default.
• W1508045386 cites W2048978054 @default.
• W1508045386 cites W2056429355 @default.
• W1508045386 cites W2057954957 @default.
• W1508045386 cites W2069594388 @default.
• W1508045386 cites W2075047310 @default.
• W1508045386 cites W2084194717 @default.
• W1508045386 cites W2086411680 @default.
• W1508045386 cites W2090679498 @default.
• W1508045386 cites W2141419570 @default.
• W1508045386 cites W2159280519 @default.
• W1508045386 cites W4251600596 @default.
• W1508045386 doi "https://doi.org/10.1016/s1874-5997(97)80009-3" @default.
• W1508045386 hasPublicationYear "1997" @default.
• W1508045386 type Work @default.
• W1508045386 sameAs 1508045386 @default.
• W1508045386 citedByCount "16" @default.
• W1508045386 countsByYear W15080453862012 @default.
• W1508045386 countsByYear W15080453862015 @default.
• W1508045386 countsByYear W15080453862016 @default.
• W1508045386 countsByYear W15080453862017 @default.
• W1508045386 countsByYear W15080453862018 @default.
• W1508045386 countsByYear W15080453862019 @default.
• W1508045386 countsByYear W15080453862023 @default.
• W1508045386 crossrefType "book-chapter" @default.
• W1508045386 hasAuthorship W1508045386A5077546710 @default.
• W1508045386 hasConcept C100951216 @default.
• W1508045386 hasConcept C109007969 @default.
• W1508045386 hasConcept C114793014 @default.
• W1508045386 hasConcept C12294951 @default.
• W1508045386 hasConcept C127313418 @default.
• W1508045386 hasConcept C13106087 @default.
• W1508045386 hasConcept C151730666 @default.
• W1508045386 hasConcept C166839181 @default.
• W1508045386 hasConcept C166957645 @default.
• W1508045386 hasConcept C17409809 @default.
• W1508045386 hasConcept C200646496 @default.
• W1508045386 hasConcept C2778697265 @default.
• W1508045386 hasConcept C2781297371 @default.
• W1508045386 hasConcept C50682988 @default.
• W1508045386 hasConcept C6494504 @default.
• W1508045386 hasConcept C95457728 @default.
• W1508045386 hasConceptScore W1508045386C100951216 @default.
• W1508045386 hasConceptScore W1508045386C109007969 @default.
• W1508045386 hasConceptScore W1508045386C114793014 @default.
• W1508045386 hasConceptScore W1508045386C12294951 @default.
• W1508045386 hasConceptScore W1508045386C127313418 @default.
• W1508045386 hasConceptScore W1508045386C13106087 @default.
• W1508045386 hasConceptScore W1508045386C151730666 @default.
• W1508045386 hasConceptScore W1508045386C166839181 @default.
• W1508045386 hasConceptScore W1508045386C166957645 @default.
• W1508045386 hasConceptScore W1508045386C17409809 @default.
• W1508045386 hasConceptScore W1508045386C200646496 @default.
• W1508045386 hasConceptScore W1508045386C2778697265 @default.
• W1508045386 hasConceptScore W1508045386C2781297371 @default.
• W1508045386 hasConceptScore W1508045386C50682988 @default.
• W1508045386 hasConceptScore W1508045386C6494504 @default.
• W1508045386 hasConceptScore W1508045386C95457728 @default.
• W1508045386 hasLocation W15080453861 @default.
• W1508045386 hasOpenAccess W1508045386 @default.
• W1508045386 hasPrimaryLocation W15080453861 @default.
• W1508045386 hasRelatedWork W1600723752 @default.
• W1508045386 hasRelatedWork W1791453176 @default.
• W1508045386 hasRelatedWork W2009103235 @default.
• W1508045386 hasRelatedWork W2074973749 @default.
• W1508045386 hasRelatedWork W2165767412 @default.
• W1508045386 hasRelatedWork W2357615465 @default.
• W1508045386 hasRelatedWork W2378348218 @default.
• W1508045386 hasRelatedWork W2383873645 @default.
• W1508045386 hasRelatedWork W2793454002 @default.
• W1508045386 hasRelatedWork W4375852613 @default.
• W1508045386 isParatext "false" @default.
• W1508045386 isRetracted "false" @default.
• W1508045386 magId "1508045386" @default.
• W1508045386 workType "book-chapter" @default.