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  • Geosyncline - Wikipedia
    A geosyncline (originally called a geosynclinal) is an obsolete geological concept to explain orogens, which was developed in the late 19th and early 20th centuries, before the theory of plate tectonics was envisaged
  • Geosyncline | Orogeny, Sedimentation Subduction | Britannica
    geosyncline, linear trough of subsidence of the Earth’s crust within which vast amounts of sediment accumulate The filling of a geosyncline with thousands or tens of thousands of feet of sediment is accompanied in the late stages of deposition by folding, crumpling, and faulting of the deposits
  • Geosyncline Theory - Geographic Book
    Geosyncline theory, also known as geosynclinal theory or geosynclinal hypothesis, was a scientific theory developed in the late 19th and early 20th centuries to explain the formation of mountain ranges and the distribution of rock formations on the Earth’s surface
  • 10. 2: Global Geological Models of the Early 20th Century
    This view incorporated a mechanism for creation of mountain chains known as the geosyncline theory A geosyncline is a thick deposit of sediments and sedimentary rocks, typically situated along the edge of a continent (Figure \(\PageIndex{1}\))
  • Geosyncline - an overview | ScienceDirect Topics
    A 'geosyncline' refers to a large accumulation of sediments and sedimentary rocks in a continental margin or basin, often incorrectly referred to as a syncline, that plays a significant role in the geological history of a region
  • Geosyncline Theory - UPSC - UPSC Notes - LotusArise
    The studies conducted during the second phase of the 20th century reveal that a geosyncline is a thick, rapidly accumulating body that lies parallel to the continent The age-old idea of a geosyncline or an intra-cratonic trough bordered by mountains contributing sediments needs to be abandoned
  • Geosyncline Theory Geosyncline Theory by Kober explains the formation . . .
    The Geosyncline Theory by Kober explains the formation of mountains and other major geological features on the earth's surface In this geography article, we will focus on the
  • Geosynclines, Mountains and Continent-Building - Scientific American
    A geosyncline is a huge deposit of sedimentary rock that forms at the edge of a continent When it is compressed, it buckles up into a mountain range It also enables a continent to
  • 地槽-地台学说 - 《中国大百科全书》第三版网络版
    研究地槽、地台的特征，发生、发展历史，以及在地壳演化中的相互关系的大地构造学说。简称槽台学说。
  • Geosynclines – GKToday
    Geosynclines can also be identified by their distinct geological features, which can include fold and thrust belts, volcanic activity, and metamorphic rocks These features are the result of the tectonic forces that shape the geosyncline, as well as the erosion and weathering that occurs over time Origins of Geosynclines





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