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首页> 外文期刊>Journal of sedimentary research >A COMPOSITIONAL CLASSIFICATION FOR GRAIN ASSEMBLAGES IN FINE-GRAINED SEDIMENTS AND SEDIMENTARY ROCKS-DISCUSSION
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A COMPOSITIONAL CLASSIFICATION FOR GRAIN ASSEMBLAGES IN FINE-GRAINED SEDIMENTS AND SEDIMENTARY ROCKS-DISCUSSION

机译:细颗粒沉积物和沉积岩中谷物组合的组成分类讨论

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摘要

Milliken's (2014) classification scheme for fine-grained sediments and sedimentary rocks is an attempt to provide an improved classification that relies on interpreted grain origin to replace existing nomenclature schemes based on sedimentary structures, grain size, and composition. Milliken posits that existing terminology is confusing and therefore proposes new terms, viz. tarl, carl, and sarl, to define three main types of mudstone categories. We consider the proposed classification impracticable because there are: (a) ambiguities associated with interpreting grain origins (intrabasinal or extrabasinal), (b) difficulties in determining the original mineralogy of diagenetically altered particles, and (c) requirements for specialized equipment and techniques not widely available to many geologists. In our opinion, the proposed classification does not improve geological understanding over prior established classification approaches.
机译:Milliken(2014)的细粒沉积物和沉积岩分类方案是一种尝试提供改进的分类方法,该方法依靠解释的晶粒起源来替代基于沉积结构,晶粒尺寸和成分的现有命名法。 Milliken认为现有术语令人困惑,因此提出了新术语,即。 tarl,carl和sarl定义三种主要类型的泥岩类别。我们认为拟议的分类是不切实际的,因为:(a)与解释谷物起源(基内或基外)相关的含糊不清;(b)确定介磁改变颗粒的原始矿物学方面的困难;以及(c)对专用设备和技术的要求不明确可供许多地质学家广泛使用。我们认为,与先前建立的分类方法相比,拟议的分类不会提高地质认识。

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