潘诺尼亚海
潘诺尼亚海(Pannonian Sea)又名副特提斯洋(Paratethys)是个史前浅海,位于现今欧洲的潘诺尼亚平原。在上新世,潘诺尼亚海的面积达到最大,并有厚达3到4公里的沉积层。
单词 | Paratethys |
释义 |
Paratethys
英汉-汉英词典
拟特提斯
词组 | 习惯用语
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Paratethys 类特提斯(古地中海边缘区地名) 网络短语:Paratethys Sea 副特提斯海
中文百科
潘诺尼亚海潘诺尼亚海(Pannonian Sea)又名副特提斯洋(Paratethys)是个史前浅海,位于现今欧洲的潘诺尼亚平原。在上新世,潘诺尼亚海的面积达到最大,并有厚达3到4公里的沉积层。
英语百科
Paratethys 潘诺尼亚海![]() ![]() The Paratethys ocean, Paratethys sea or just Paratethys was a large shallow sea that stretched from the region north of the Alps over Central Europe to the Aral Sea in Central Asia. The sea was formed during the Oxfordian stage of the Late Jurassic as an extension of the rift that formed the Central Atlantic Ocean and was isolated during the Oligocene epoch (about 34 million years ago). It was separated from the Tethys Ocean to the south by the formation of the Alps, Carpathians, Dinarides, Taurus and Elburz mountains. During its long existence the Paratethys was at times reconnected with the Tethys or its successors, the Mediterranean Sea or Indian Ocean. From the Pliocene epoch onward (after 5 million years ago), the Paratethys became progressively shallower. Today's Black Sea, Caspian Sea, Aral Sea, Lake Urmia and others are remnants of the Paratethys Sea. |
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