潮汐海峡沉积模式修正

IF 10 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Sergio G. Longhitano
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引用次数: 0

摘要

本文以2013年发表的原型为基础,提出了一个修正的潮汐海峡沉积模型。该模型将潮汐海峡细分为四个主要区域:(a)海峡中心区,(B)沙丘层状区,(C)海峡末端区,(D)海峡边缘区,这表明每个区域都是根据其独特的水动力、沉积结构和粒度分布来识别的。该模型还提供了预测沉积柱和主要地层格架,可用于识别保存在露头或地下的古海峡充填序列。虽然它标志着对现代和古代潮汐海峡的了解取得了重大进展,但它的适用性受到其所依据的案例研究数量有限的限制。本文提出的新模式整合了29个现代和22个古代潮汐海峡的见解,以加强对海峡尺度沉积过程及其地层特征的认识。修订后的框架重申了四个主要沉积带的存在,但引入了一些新的元素,包括:(i)在A区也认识到沉积相,如砾石带,以前被认为是唯一的旁路环境;(ii)作为水流主导的潮汐沉积早期过程前兆的超临界流构造的存在;(iii) B区的河床种类扩大,包括潮沙脊;C带浅水潮汐过程与较深的含钙岩矿床之间的新联系;(5)将海峡边缘或d带的三角洲变形和沉积物改造纳入该模型,并结合具体的鱼相类型,为识别岩石记录中的古潮汐海峡提供了更好的地层标准,并强调了它们与古地理重建和地下资源勘探的相关性。最后,该研究确定了现代海峡中具有潮汐和波浪能量收集潜力的关键区域,强调了潮汐海峡对可持续能源战略的更广泛影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tidal strait depositional model revised
This paper presents a revised depositional model for tidal straits, building upon a previous prototype published in 2013. That model introduced a subdivision of tidal straits into four main sectors: (A) a strait-center, (B) a dune-bedded zone, (C) strait-end zone, and (D) a strait-margin zone, indicating as each of these zones are identifiable based on their distinctive hydrodynamics, sedimentary structures, and grain-size distributions. The model also provided predictive sedimentological columns and a main stratigraphic framework useful for the identification of ancient strait-fill successions preserved in outcrop or subsurface. While it marked a significant advancement in the understanding of both modern and ancient tidal straits, its applicability was constrained by the limited number of case studies on which it was based.
The new model presented in this paper integrates insights from 29 modern and 22 ancient tidal straits to enhance the understanding of strait-scale sedimentary processes and their stratigraphic signatures. The revised framework reaffirms the presence of the four principal depositional zones but introduces some novel element, including: (i) the recognition of sedimentary facies also in Zone A, such as gravel ribbons, previously considered as a sole bypass environment; (ii) the presence of supercritical-flow structures as an early process precursor of current-dominated tidal sedimentation; (iii) an expanded variety of bedforms in Zone B, including tidal sand ridges; (iv) a new link between shallow-water tidal processes and deeper contouritic deposits in Zone C; and (v) the inclusion of delta deflection and sediment reworking along strait margins or Zone D. The updated model additionally offers improved stratigraphic criteria for recognizing ancient tidal straits in the rock record, integrated with specific types of ichnofacies, and emphasizes their relevance to paleogeographic reconstructions and subsurface resource exploration. Finally, the study identifies key areas within modern straits with potential for tidal and wave energy harvesting, highlighting the broader implications of tidal straits for sustainable energy strategies.
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来源期刊
Earth-Science Reviews
Earth-Science Reviews 地学-地球科学综合
CiteScore
21.70
自引率
5.80%
发文量
294
审稿时长
15.1 weeks
期刊介绍: Covering a much wider field than the usual specialist journals, Earth Science Reviews publishes review articles dealing with all aspects of Earth Sciences, and is an important vehicle for allowing readers to see their particular interest related to the Earth Sciences as a whole.
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