P. H. Cornard, G. Degenhart, P. Tropper, J. Moernaut, M. Strasser
{"title":"应用微型计算机断层扫描技术解析深海砂岩的纹理特性并评估其原始沉积结构","authors":"P. H. Cornard, G. Degenhart, P. Tropper, J. Moernaut, M. Strasser","doi":"10.1002/dep2.261","DOIUrl":null,"url":null,"abstract":"<p>Over the past decade, there has been growing interest in the sedimentological community to use micro X-ray computed tomography to analyse microfacies in sediment cores. However, little attention has been paid to the application of micro-computed tomography in lithified deposits, even though this can allow their texture to be characterised in three dimensions, providing key information about sedimentary structures. A novel application of micro-computed tomography in lithified sediment-gravity flow deposits is presented with the objective of characterising their internal 3D sedimentary structures. This technique is applied to three deep-marine sandstones showing different compositional properties: Cretaceous Gosau Group (Austria), Eocene Hecho Group (Spain) and the Oligocene Annot Formation (France). From micro-computed tomography data the size of particles and their distribution throughout the sample is reconstructed in 3D permitting a better visualisation of sedimentary textures. Particle distributions computed from micro-computed tomography are similar to those computed from thin section image analysis, corroborating the reliability of the micro-computed tomography to evaluate grain-size trends. Micro-computed tomography is complemented with micro-X-ray fluorescence and thin section petrographic analyses. In cases where mineral composition or grain size are homogeneous or matrix and grains have similar mineral composition, sedimentary structures do not appear visible from micro-X-ray fluorescence or thin section analyses. By separating particles based on their computed tomography density, it is possible to isolate the coarsest fraction, highlighting the sedimentary structures. This study demonstrates (i) the potential of micro-computed tomography in analyses of sedimentary structures from outcrop data and (ii) the importance of the mineralogical composition and degree of grain sorting in assessing the origin of structureless deposits. Considering the importance of visualising sedimentary structures when interpreting depositional processes, micro-computed tomography is a new and reliable tool to assess the physical properties of sandstones and to analyse their internal 3D sedimentary structures.</p>","PeriodicalId":54144,"journal":{"name":"Depositional Record","volume":"10 5","pages":"559-580"},"PeriodicalIF":1.9000,"publicationDate":"2023-12-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/dep2.261","citationCount":"0","resultStr":"{\"title\":\"Application of micro-CT to resolve textural properties and assess primary sedimentary structures of deep-marine sandstones\",\"authors\":\"P. H. Cornard, G. Degenhart, P. Tropper, J. Moernaut, M. 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From micro-computed tomography data the size of particles and their distribution throughout the sample is reconstructed in 3D permitting a better visualisation of sedimentary textures. Particle distributions computed from micro-computed tomography are similar to those computed from thin section image analysis, corroborating the reliability of the micro-computed tomography to evaluate grain-size trends. Micro-computed tomography is complemented with micro-X-ray fluorescence and thin section petrographic analyses. In cases where mineral composition or grain size are homogeneous or matrix and grains have similar mineral composition, sedimentary structures do not appear visible from micro-X-ray fluorescence or thin section analyses. By separating particles based on their computed tomography density, it is possible to isolate the coarsest fraction, highlighting the sedimentary structures. 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引用次数: 0
摘要
过去十年来,沉积学界对使用微型 X 射线计算机断层扫描技术分析沉积岩芯中的微地貌越来越感兴趣。然而,人们很少关注在岩化沉积物中应用微型计算机断层扫描技术,尽管这种技术可以从三维角度描述岩化沉积物的纹理特征,提供有关沉积结构的关键信息。本文介绍了微计算机断层扫描技术在岩化沉积-重力流沉积中的新应用,目的是描述其内部三维沉积结构的特征。该技术应用于三种具有不同成分特性的深海砂岩:它们分别是白垩纪戈绍组(奥地利)、始新世海乔组(西班牙)和渐新世安诺特地层(法国)。通过微观计算机断层扫描数据,可对颗粒大小及其在整个样本中的分布情况进行三维重建,从而更好地观察沉积纹理。通过微型计算机断层扫描计算出的颗粒分布与通过薄片图像分析计算出的颗粒分布相似,这证实了微型计算机断层扫描评估颗粒大小趋势的可靠性。显微 X 射线荧光和薄片岩相分析是对显微计算机断层扫描的补充。在矿物成分或晶粒大小均一或基质和晶粒的矿物成分相似的情况下,沉积结构在显微 X 射线荧光或薄片分析中并不明显。根据计算机断层扫描密度分离颗粒,可以分离出最粗的部分,突出沉积结构。这项研究证明了(i)微型计算机断层扫描技术在从露头数据分析沉积结构方面的潜力,以及(ii)矿物成分和颗粒分选程度在评估无结构矿床起源方面的重要性。考虑到在解释沉积过程时可视化沉积结构的重要性,显微计算机断层扫描是评估砂岩物理特性和分析其内部三维沉积结构的可靠新工具。
Application of micro-CT to resolve textural properties and assess primary sedimentary structures of deep-marine sandstones
Over the past decade, there has been growing interest in the sedimentological community to use micro X-ray computed tomography to analyse microfacies in sediment cores. However, little attention has been paid to the application of micro-computed tomography in lithified deposits, even though this can allow their texture to be characterised in three dimensions, providing key information about sedimentary structures. A novel application of micro-computed tomography in lithified sediment-gravity flow deposits is presented with the objective of characterising their internal 3D sedimentary structures. This technique is applied to three deep-marine sandstones showing different compositional properties: Cretaceous Gosau Group (Austria), Eocene Hecho Group (Spain) and the Oligocene Annot Formation (France). From micro-computed tomography data the size of particles and their distribution throughout the sample is reconstructed in 3D permitting a better visualisation of sedimentary textures. Particle distributions computed from micro-computed tomography are similar to those computed from thin section image analysis, corroborating the reliability of the micro-computed tomography to evaluate grain-size trends. Micro-computed tomography is complemented with micro-X-ray fluorescence and thin section petrographic analyses. In cases where mineral composition or grain size are homogeneous or matrix and grains have similar mineral composition, sedimentary structures do not appear visible from micro-X-ray fluorescence or thin section analyses. By separating particles based on their computed tomography density, it is possible to isolate the coarsest fraction, highlighting the sedimentary structures. This study demonstrates (i) the potential of micro-computed tomography in analyses of sedimentary structures from outcrop data and (ii) the importance of the mineralogical composition and degree of grain sorting in assessing the origin of structureless deposits. Considering the importance of visualising sedimentary structures when interpreting depositional processes, micro-computed tomography is a new and reliable tool to assess the physical properties of sandstones and to analyse their internal 3D sedimentary structures.