陆表海(epeiric sea)：又称内陆海、陆内海、大陆海，是位于大陆内部或陆棚内部的，低海底坡度(30m,多为几百米)，太暗。底部水体停滞缺氧，来自周围陆棚的底流可为超盐度，较大密度，不易上流所致。
本文提出了内陆表海含煤盆地层序界面类型和层序模式。
This paper puts forward the types of sequence stratigraphic boundary and the sequence stratigraphic model bf epicontinental basin.
研究区晚古生代含煤岩系主要形成于陆表海—海岸平原环境中。
In the research area, the coal series in late Palaeozoic era were mainly formed from epeiric sea - coastal plain environment.
华南陆表海沉积与生物的发育深受其东南边缘茅口期以来隆起成陆的影响。
Depositional agent and biological action in the east part of the South China epicontinental sea are chiefly controlled by the land upliffting of its southeastern edge since theMaokouan Stage.
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