Tidal Modulated Shoreface Facies in Eocene Agbada Formation, Niger Delta Basin, Nigeria

Abraham. O. Opatola, Saheed A. Alli
{"title":"Tidal Modulated Shoreface Facies in Eocene Agbada Formation, Niger Delta Basin, Nigeria","authors":"Abraham. O. Opatola, Saheed A. Alli","doi":"10.47524/tjst.v4i1.24","DOIUrl":null,"url":null,"abstract":"Tidal influence shoreface are shoreface deposit generated by wave induced tidal action. The extent of the tidal impact from lower to upper shorefaces depend mostly on the tidal range thereby controlling the impact of different shoreline wave action on sediment distribution across shorefaces. The Tidally influenced shoreface sediment display wave generated structure, however the structure are strongly associated with tidal generated structures and trace fossil consistent with tidal depositional setting. Shoreface successions in Titun well display a wide range of variability, largely restricted to the lower and middle shoreface intervals. This variation was controlled by relative wave dominance and intermittent pulsating nature of associated tidal bed deposition. The successions were subdivided into three end members, although a complete gradation between them exists. High energy shoreface consist almost entirely of erosively based amalgamated tide and wave beds with minimal bioturbation. Intermediate energy shoreface consist of stacked laminated to burrowed intervals, recording repeated erosive storm bed emplacement, followed by opportunistic colonization, and commonly overprinted by resident fairweather burrowing. Weakly storm-affected low energy shorefaces typically show intense bioturbation with minimal preservation of high energy beds. Based on the association of the facies, facies vertical build-up patterns, sedimentary structures and trace fossil content, the T1 sands in Titun well are interpreted as a prograding tidally influence shoreface deposit. This interpretation is supported by presence of tide generated structures and marine trace fossil, due to the prevalence of several tidal imprint as suggested by several mud drapes and flasers, couplets of sands and shale’s in heterolithic sequences, and bidirectional current structures (herringbone cross stratification), a tidally influence shoreface geological model is suggested for deposit.","PeriodicalId":17491,"journal":{"name":"Journal of Tropical Animal Science and Technology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Tropical Animal Science and Technology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.47524/tjst.v4i1.24","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Tidal influence shoreface are shoreface deposit generated by wave induced tidal action. The extent of the tidal impact from lower to upper shorefaces depend mostly on the tidal range thereby controlling the impact of different shoreline wave action on sediment distribution across shorefaces. The Tidally influenced shoreface sediment display wave generated structure, however the structure are strongly associated with tidal generated structures and trace fossil consistent with tidal depositional setting. Shoreface successions in Titun well display a wide range of variability, largely restricted to the lower and middle shoreface intervals. This variation was controlled by relative wave dominance and intermittent pulsating nature of associated tidal bed deposition. The successions were subdivided into three end members, although a complete gradation between them exists. High energy shoreface consist almost entirely of erosively based amalgamated tide and wave beds with minimal bioturbation. Intermediate energy shoreface consist of stacked laminated to burrowed intervals, recording repeated erosive storm bed emplacement, followed by opportunistic colonization, and commonly overprinted by resident fairweather burrowing. Weakly storm-affected low energy shorefaces typically show intense bioturbation with minimal preservation of high energy beds. Based on the association of the facies, facies vertical build-up patterns, sedimentary structures and trace fossil content, the T1 sands in Titun well are interpreted as a prograding tidally influence shoreface deposit. This interpretation is supported by presence of tide generated structures and marine trace fossil, due to the prevalence of several tidal imprint as suggested by several mud drapes and flasers, couplets of sands and shale’s in heterolithic sequences, and bidirectional current structures (herringbone cross stratification), a tidally influence shoreface geological model is suggested for deposit.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
尼日利亚尼日尔三角洲盆地始新统Agbada组潮汐调制滨相
潮汐影响岸面是由波浪诱发潮汐作用而形成的岸面沉积。潮汐从下到上的影响程度主要取决于潮差,从而控制了不同岸线波浪作用对各岸面沉积物分布的影响。受潮影响的滨面沉积物表现为波生构造,但该构造与潮生构造密切相关,且遗迹化石与潮生沉积环境一致。图顿井的岸面层序表现出很大的变异性,主要局限于中下部岸面层段。这种变化受相对波浪优势和伴生潮床沉积的间歇脉动性质控制。序列被细分为三个端元,尽管它们之间存在完整的级配。高能滨面几乎完全由侵蚀性混合的潮床和波床组成,生物扰动最小。中等能量的岸面由层叠的层状到挖洞的间隔组成,记录了反复侵蚀的风暴床位置,随后是机会性的殖民化,通常被居民的fairweather挖洞覆盖。弱风暴影响的低能岸面通常表现出强烈的生物扰动,高能量层的保存最少。根据相组合、相垂向堆积模式、沉积构造和微量化石含量,将土屯井T1砂解释为潮汐作用的进动滨面沉积。潮生构造和海相痕迹化石的存在支持了这一解释,由于几个泥幔和闪光的潮汐印记的存在,异质层序中砂和页岩的对联,以及双向流构造(人字交叉层理),提出了潮汐影响的滨面地质模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Chemical Characteristics of cull Ongole Beef Sausage with Substitution of Tapioca and Soy Bean Flour Nutrient Adequacy of Beef Cattle in Coastal Areas Kumai Sub-District, West Kotawaringin District Goat Performance of Peanut Goat with Supplementation of Feed Wafers Containing Lamtoro Taramba Leaves at Sumbawa Global Farm Reproductive Organ Profile of Pullet Phase Kampung Chicken After L-Isoleucine Supplementation in Feed Anti-Oxidant and Vitamin C Activity Test of Horseganik Clay Mask Products, Sumbawa Horse Milk
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1