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- W2374927220 abstract "Abu Gabra Formation of Cretaceous Fula depression, which is formed during the first rifting cycle, can be divided into three second-order sequences, namely, sequence K1SSI, sequence K1SSⅡ and sequence K1SSⅡI. They can correspond separately to the strata deposited in the early, middle and late rift period. Of the three second-order sequences, the sequence K1SSI and sequence K1SSⅡI can be subdivided into two third-order sequences, the sequence K1SSⅡ into three third-order sequences. Based on the integrated analysis of seismic data, core and well logging, the distribution of sedimentary facies and the prediction of sedimentary system are achieved. Through investigation, 7 types of sedimentary facies are recognized, namely, fluvial deposit, delta, fan delta, braided delta, proximal sublacustrine fan, lacustrine facies. Due to the evolution of their sedimentary facies, five chief depositional systems are established in the Fula depression. They are fan delta system in the NE, delta system in the NW, proximal sub-lacustrine fan in the west, braided delta system in the ES and fluvial system produced in the early period. The distribution and evolution of the depositional systems is controlled by tectonics, probably influenced by paleotopography and paleogeography." @default.
- W2374927220 created "2016-06-24" @default.
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- W2374927220 date "2008-01-01" @default.
- W2374927220 modified "2023-09-26" @default.
- W2374927220 title "Lower Cretaceous Sequence Stratigraphy of Fula Depression,Muglad Basin,Sudan" @default.
- W2374927220 hasPublicationYear "2008" @default.
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