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Geological-Geomorphological Structure and Recent History of the Iranian Coast of the Caspian Sea

机译:里海伊朗海岸的地质-地貌结构和近期历史

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摘要

The Iranian coast of the Caspian Sea is an element of the South Caspian Depression, which represents a spacious plain with a subtropical climate bordered in the south by the Elburs mountainous system. Its western, central, and eastern parts bear different names: Gilyan, Mazandaran, and Golestan plains, respectively. In structural terms, this region represents the Elburs foredeep filled with a thick sequence of Neo-gene-Quaternary sediments and separated from the Elburs fold system by a deep-seated regional fault.
机译:里海的伊朗海岸是南里海De陷的一个组成部分,它代表着一个宽阔的平原,南部是亚热带气候,与埃尔伯斯山区系统接壤。其西部,中部和东部分别具有不同的名称:吉利安,马赞丹兰和戈列斯坦平原。从结构上讲,该区域代表前额Elburs深处,充满了厚厚的新近纪第四纪沉积物序列,并通过深部区域性断层与Elburs褶皱系统隔开。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|843-848|共6页
  • 作者单位

    Department of Geography, Moscow State University, Vorob'evygory, Moscow, Russia;

    Department of Geography, Moscow State University, Vorob'evygory, Moscow, Russia;

    Department of Geography, Moscow State University, Vorob'evygory, Moscow, Russia;

    Department of Geography, Moscow State University, Vorob'evygory, Moscow, Russia;

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