Cretaceous paleogeography in China
Cretaceous paleogeography in China
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DOI：
10.1016/0031-0182(87)90073-3
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发表时间：
1987
期刊：
影响因子：
--
通讯作者：
Pei-ji Chen
中科院分区：
文献类型：
--
作者：
Pei-ji Chen
中国的古地理由四幅地图表示：Neocomian，Aptian-Albian，Cenomanian-Santonian和Campanian-Maastrichtian。中国大陆内部的特点是构造洼地和山间盆地中的大型湖泊系统，很少或没有海洋影响。白垩纪陆表海受青藏高原东部边缘和南部、西部构造槽的限制。与中国白垩纪内陆沉积的详细知识相比，海洋入侵的记录仅以一般的方式被了解。
The paleogeography of China is represented by four maps: the Neocomian, Aptian-Albian, Cenomanian-Santonian, and the Campanian-Maastrichtian. The continental interior of China was characterized by large lake systems in tectonic depressions and intermontane basins, with little or no marine influence. Shallow epicontinental Cretaceous seas were limited by the eastern margins and to the tectonic troughs of the southern and western Tibetan Plateau. In contrast to the detailed knowledge of the interior Cretaceous deposits of China, the record of the marine invasions is known only in a general way.