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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:在十八世纪,意大利发生了对自然环境和尤其是地质的研究。山脉组成和形成的新概念以及地球的结构从区域实地调查岩石,地貌及其相对位置的岩性和古生物学研究。在佛罗伦萨科学家N. Steno基础地质基础原则的关键洞察力之后,形成山脉和岩石的分类迅速发展。从该分类,基于岩石的位置和相对性质的相对年度学的形式逐渐出现广泛的地层序列系统。这导致了“初级”(或“原始”),“二次”和“三级”的术语提出,以描述山脉的性质,并因此开始用作地层单位。在威尼斯和托斯卡纳山区的二十几十年的野外工作之后,在十八世纪中叶,采矿工程师和野外地质学家Giovanni Arduino在意大利北部的山地和岩石的分类时作出了显着的贡献。他的计划将山脉和岩石分成了四个基本单位或“德尼尼”,基于岩性,位置和内部结构,但排除了化石证据。三个山脉和四分之一的平原,分别:“主要”(由“原始”或Primaeval“Schist被认为是最早的岩石),”二次“和”三级“。他最年轻的师,“四阶”或“Quarto Orate”包括强烈的和河口沉积物,河谷或平原。他对“第四阶”的认可是第一次签署代表第四纪的存款并定义为离散序列。通过这种方式,Arduino的分类系统奠定了现代地层的基础。

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