Seismic expression of shallow-water carbonate structures through geologic time

Marcello Badali’
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Abstract

Shallow-water carbonate structures are characterized by different shapes, sizes and identifying features, which depend, among other factors, on the age of deposition and on the carbonate factory associated with a specific geologic period. These variations have a significant impact on the imaging of these structures in reflection seismic data. This study aims at providing an overall, albeit incomplete, picture of how the seismic expression of shallow-water carbonate structures has evolved through deep time. 297 shallow-water carbonate systems of different ages, spanning from Precambrian to present, with a worldwide distribution of 159 sedimentary basins, have been studied. For each epoch, representative seismic examples of shallow-water carbonate structures were described through the assessment of a selection of discriminating seismic criteria, or parameters. The thinnest structures, commonly represented by ramp systems, usually occurred after mass extinction events, and are mainly recognizable in seismic data through prograding clinoform reflectors. The main diagnostic seismic features of most of the thickest structures, which were found to be Precambrian, Late Devonian, Middle-Late Triassic, Middle-Late Jurassic, some Early Cretaceous pre-salt systems, #8220;middle#8221; and Late Cretaceous, Middle-Late Miocene and Plio-Pleistocene, are steep slopes, and reefal facies. Slope-basinal, resedimented seismic facies, were mostly observed in thick, steep-slope platforms, and they are more common, except for megabreccias, in post-Triassic structures. Seismic-scale, early karst-related dissolution features were mostly observed in icehouse, platform deposits. Pinnacle structures and the thickest margin rims are concentrated in a few epochs, such as Middle-Late Silurian, Middle-Late Devonian, earliest Permian, Late Triassic, Late Jurassic, Late Paleocene, Middle-Upper Miocene, and Plio-Pleistocene, which are all characterized by high-efficiency reef builders.
浅水碳酸盐结构在地质年代中的地震表现形式
浅水碳酸盐结构具有不同的形状、大小和识别特征,除其他因素外,还取决于沉积年龄和与特定地质时期相关的碳酸盐工厂。这些变化对这些结构在反射地震数据中的成像有重大影响。本研究的目的是对浅水碳酸盐结构的地震表达如何随着深部时间的推移而演变提供一个整体的描述,尽管并不完整。研究了 297 个不同时代的浅水碳酸盐系统,时间跨度从前寒武纪到现在,分布于全球 159 个沉积盆地。在每个时代,通过评估选定的地震判别标准或参数,描述了浅水碳酸盐结构的代表性地震实例。最薄的结构通常以斜坡系统为代表,通常发生在大灭绝事件之后,在地震数据中主要通过渐变的基诺形反射体来识别。大多数最厚构造的主要地震诊断特征是陡坡和暗礁面,这些构造被发现属于前寒武纪、晚泥盆世、中晚三叠世、中晚侏罗世、部分早白垩世前盐系、#8220;中#8221;和晚白垩世、中晚中新世和上新世。斜坡基底、沉积地震面主要出现在厚陡坡平台上,在后三叠纪构造中,除巨型砾岩外,斜坡基底、沉积地震面更为常见。地震尺度的早期岩溶溶蚀特征主要出现在冰室、平台沉积中。尖顶结构和最厚的边缘边缘集中在几个纪,如志留纪中-晚期、泥盆纪中-晚期、二叠纪早期、三叠纪晚期、侏罗纪晚期、古新世晚期、中新世中-上新世和上新世-始新世,这些纪都具有高效造礁的特征。
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