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| DOI | 10.1016/j.earscirev.2018.12.014 |
| Petrographic classification of sand and sandstone | |
| Garzanti E. | |
| 发表日期 | 2019 |
| ISSN | 00128252 |
| 起始页码 | 545 |
| 结束页码 | 563 |
| 卷号 | 192 |
| 英文摘要 | Petrographic classifications of sand and sandstone proposed more than half a century ago are still in use, although they were formulated at a time when depositional and post-depositional sedimentary processes were poorly understood, and before the relationships between tectonics and sedimentation could be interpreted in modern plate-tectonic terms. As a consequence, too many scientific articles and technical reports are still encumbered with obsolete concepts, graphical tools, and ambiguous terminology that make sediment descriptions awkward and misleading. A renovation that treasures the legacy of the pioneers is required. The descriptive petrographic classification of sand and sandstone proposed in this paper is based on the quasi-universally used Gazzi-Dickinson point-counting method, and simply translates into words ternary compositions of quartz, feldspar, and lithic fragments without introducing any new names. The classic QFL plot is subdivided into 15 fields - labelled by adjectives introduced long ago by K.A.W. Crook and endorsed by W.R. Dickinson and more recently by G.J. Weltje - which reflect relative abundances of the three main framework components (provided they exceed 10%QFL). According to standard use, the less abundant component goes first, the more abundant last (e.g., litho-feldspatho-quartzose composition translates into Q > F > L > 10%QFL). For lithic-rich sand and sandstone, information on the prevailing rock fragment type can be added by an additional free adjective (e.g., metamorphiclastic, carbonaticlastic), as proposed long ago by R.V. Ingersoll. For lithic-poor feldspatho-quartzose and quartzose sand and sandstone, further formal subdivisions are proposed based on the Q/F ratio, thus reaching a total of 18 compositional fields overall. Modern sand known to be derived from different source rocks and found in major world's rivers, deserts, and deep-sea fans fits in the pigeonholes defined by the relative abundance of quartz, feldspar, and lithic fragments. The aim of this classification is to restore directness in sandstone petrology, and to avoid ambiguities generated in the past by making reference to badly defined archetypes, such as greywacke or arkose, thus confusing petrographic composition with subjective considerations about plate-tectonic setting, texture, hydraulic behaviour, mechanical durability, or chemical durability in the illusion that a classification could be genetic at the same time as descriptive. © 2018 Elsevier B.V. |
| 关键词 | Chert, carbonate, and evaporite grainsClassification of modern river, turbidite, and desert sandGazzi-Dickinson methodGreywacke and arkosePlate-tectonic settingQFL diagramRock fragmentsSandstone petrologySediment provenanceTexture and composition |
| 英文关键词 | carbonate; chert; classification; evaporite; graywacke; petrography; petrology; plate tectonics; sand; sandstone; sedimentation; Gorgonacea |
| 语种 | 英语 |
| 来源期刊 | Earth Science Reviews
 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/203430 |
| 作者单位 | Laboratory of Provenance Studies, Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milano, Italy |
| 推荐引用方式 GB/T 7714 | Garzanti E.. Petrographic classification of sand and sandstone[J],2019,192. |
| APA | Garzanti E..(2019).Petrographic classification of sand and sandstone.Earth Science Reviews,192. |
| MLA | Garzanti E.."Petrographic classification of sand and sandstone".Earth Science Reviews 192(2019). |
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