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首页> 外文期刊>Journal of Environment and Earth Science >Paleodepositional Environment and Sequence Stratigraphy of Outcropping Sediments in Parts of Southern Middle Niger Basin, Nigeria
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Paleodepositional Environment and Sequence Stratigraphy of Outcropping Sediments in Parts of Southern Middle Niger Basin, Nigeria

机译:尼日利亚尼日尔中南部盆地部分地区露头沉积环境的古沉积环境和层序地层

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The determination of paleodepositional environment and sequence stratigraphic framework within which geologic factors interplayed to create the sedimentary facies present in outcropping sediments in parts of the Southern Middle Niger Basin, in order to establish sedimentary architectures and chronostratigraphically significant surfaces; erecting a stratigraphic framework through quantitative palynological and sedimentological analysis of sediments by detailed field mapping and laboratory techniques, forms the focus of this study. The Lokoja Formation was mapped on outcrops exposed in Robinson Street, Mount Patti, Banda and Filele in Lokoja area, while the Patti Formation was mapped in Ahoko, Gegu Beki, Gegu Egba, Adabor, Orehi and Akpasi along the Lokoja-Abuja express way. The study area lies within Latitude N 070 81’ and N 080 30’; Longitude E 0060 73’ and E 0060 86’. Three main lithofacies, sand, shale and silt were defined with seven subfacies as silty sand, fine-grained sand, medium-grained sand, coarse-grained sand, clayey siltstone, silty clay, and sandy silt. Sorting ranged from 0.72 – 1.29, indicating poor – moderate sorting for the Lokoja Formation. Depositional environments defined by values of binary plots of skewness versus standard deviation and mean versus standard deviation for samples obtained from the Lokoja area, confirmed by binary plot of skewness versus median for same samples indicate a continental fluvial and shallow marine to transitional paleodepositional environment for the Lokoja Formation and the Patti Formation respectively. Three systems tracts, LST, TST and HST, were established in the study with the Lokoja Formation as an LST, the lower section of the Patti as a TST and the upper section as an HST. An SB and a candidate MFS of probably Late Cretaceous age was established at the base of the Lokoja Formation and in the Patti Formation respectively. Age-significant Cretaceous palynomorph species recovered from the Patti Formation which includes Cyathidites sp., Monocolpopollenites spheroidites, Proteacidites dehanni, P. longispinosus, Cingulatosporites ornatus, Echitriporites triangulatus, Baculatisporites sp., Longapetites veneendenburgi, and Monocolpites marginatus indicate and confirm a Late Cretaceous age for the Patti Formation. Keywords: Sequence stratigraphy, Middle Niger Basin, Patti Formation, Lokoja Formation, Depositional Environment.
机译:确定古沉积环境和层序地层格架,在其中地质因素相互影响,以形成尼日尔中南部盆地部分露头沉积物中存在的沉积相,以建立沉积构造和地层地层;通过详细的野外测绘和实验室技术对沉积物进行定量的孢粉学和沉积学分析来建立地层框架,是本研究的重点。 Lokoja组被绘制在位于Lokoja地区罗宾逊街,帕蒂山,班达和Filele露头的露头上,而Patti组则沿着Lokoja-Abuja高速公路被绘制在Ahoko,Gegu Beki,Gegu Egba,Adabor,Orehi和Akpasi上。研究区域位于Latitude N 070 81'和N 080 30'之内;经度E 0060 73'和E 0060 86'。定义了三个主要岩相,分别为砂,页岩和粉砂,分为粉砂,细粒砂,中粒砂,粗粒砂,黏土粉砂岩,粉质粘土和砂质粉砂七个亚相。排序范围为0.72-1.29,表明Lokoja组的排序较差-中度。由Lokoja地区获得的样品的偏度与标准偏差,均值与标准偏差的二元图的值定义的沉积环境,由相同样品的偏度与中值的二元图证实,表明该地区为陆相河流相和浅海相向过渡古沉积环境。 Lokoja组和Patti组。在研究中建立了三个系统区域,LST,TST和HST,以Lokoja组为LST,以Patti的下部为TST,以上部为HST。在Lokoja组的底部和Patti组分别建立了可能为白垩纪晚期的SB和候选MFS。从帕蒂组中发现的具有年龄意义的白垩纪古物形态包括Cyathidites sp。,Monocolpopollenites spheroidite,Proteacidites dehanni,P。longispinosus,Cingulatosporites ornatus,Echitriporites triangulatus,Baculatisporites sp。,Longapetus vcolendretatage和为帕蒂编队。关键词:层序地层,尼日尔中部盆地,Patti组,Lokoja组,沉积环境。

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