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Giovanni Arduino - the man who invented the Quaternary

机译:Giovanni Arduino-发明第四纪的人

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A flowering of research into the natural environment and particularly geology took place in Italy in the eighteenth century. New concepts of the composition and formation of mountains and the structure of the Earth arose from regional field investigation of the lithology and palaeontology of the rocks, geomorphology and their relative position. Classification of mountains and the rocks from which they were formed developed rapidly following the critical insights into basic geological foundation principles by the Florentine scientist N. Steno. From this classification, a broad system of stratigraphical sequence gradually emerged in the form of a relative chronology based on the position and relative properties of the rocks. This led to the proposal of the terms "primary" (or "primitive"), "secondary," and "tertiary" to describe the nature of mountains and in addition the terms began to be used as stratigraphic units. By the middle of the eighteenth century, the mining engineer and field geologist Giovanni Arduino, following two decades of fieldwork in the Venetian and Tuscan mountains, made a remarkable contribution when he proposed a classification of mountain and rocks in northern Italy. His scheme divided the mountains and rocks into four basic units or "ordini" which were based on lithology, position and internal structure, yet excluded fossil evidence. The three orders of mountains and a fourth of the plains, were respectively: "Primary" (underlain by "Primitive or Primaeval" schist considered to be the earliest rocks), "Secondary" and "Tertiary". His youngest division, the "Fourth Order" or "Quarto orate" comprised alluvial and estuarine deposits that underlie river valleys or plains. His recognition of the "Fourth Order" was the first time that deposits representing the Quaternary had been identified and defined as a discrete sequence. In this way, Arduino's classification system of divisions laid the foundations of modern stratigraphy.
机译:在18世纪的意大利,对自然环境特别是地质学的研究蓬勃发展。山的组成和形成以及地球结构的新概念来自岩石的岩性和古生物学,地貌及其相对位置的区域野外调查。在佛罗伦萨科学家N. Steno对基本地质基础原理进行了批判性洞察之后,对形成山脉和山脉的岩石的分类迅速发展。通过这种分类,基于岩石的位置和相对性质,以相对年表的形式逐渐出现了广泛的地层层序体系。这导致提出了术语“主要”(或“原始”),“次要”和“第三级”来描述山脉的性质,此外,这些术语开始被用作地层单位。到18世纪中叶,采矿工程师和现场地质学家Giovanni Arduino在威尼斯人和托斯卡纳山区进行了二十年的实地考察之后,提出了意大利北部山区和岩石分类的杰出贡献。他的计划将山脉和岩石分为四个基本单位,即“ ordini”,这两个基本单位是基于岩性,位置和内部结构的,但不包括化石证据。三级山脉和四分之一的平原分别是:“ Primary ”(在“ Primitive或Primaeval ”片岩中被认为是最早的岩石),“ Secondary ”和“ Tertiary ” 。他最年轻的部门是“第四级”或“四分之四”,由位于河谷或平原下面的冲积和河口沉积物组成。他对“第四阶”的认识是首次确定代表第四纪的沉积并将其定义为离散序列。这样,Arduino的部门分类系统为现代地层学奠定了基础。

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