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埕岛油田是我国投入开发的第一个浅海整装大油田。Chengdao oilfield is the first developed epicontinental sea monoblock oilfield.

在东亚的陆缘地区。存在着一系列的陆缘弧。There are a series of epicontinental ares in the marginal regions of the East Asia.

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滨海区的志留系，已成为兴凯地体陆缘增生带的组成部分。TheSilurian on the littoral area has been a part of the Xingkai terrain epicontinental aggradation-al belt.

研究表明塔中志留系为陆表海碎屑潮坪沉积。Studies showed that the Silurian sytem in the Tazhong area was deposited in an epicontinental sea tidal flat environment.

原岩形成于相对稳定的大陆边缘-微板块内的陆表海环境。The source rock could be formed in the condition of relatively stable continental margin epicontinental marine in micro-plate.

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.

以层序地层学概念，探讨石炭纪的下扬子盆地—陆表海盆地。The paper deals with the Carboniferous of Lower Yangtze Basin- an epicontinental basin based on the principle of sequence stratigraphy.

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重点探讨了我目东南沿海陆缘弧的重力异常特征及其形成机割。The features and their original mechanism of gravity anomaly of the epicontinental arc in the Southeast China are the focal point in discussion.

晚石炭世，贺兰山一带形成裂陷海湾沉积，而中央古隆起以东则广泛发育陆表海沉积。In the late Carboniferous, rift bay deposit occurred in Helanshan, while widespread epicontinental sea deposit developed in the area east of paleo-mid-ridge.

运用马尔柯夫链随机性教学模型对研究区陆表海盆地沉积序列特性进行了分析研究。The feature of the sedimentary succession of the epicontinental sea basin in the study area was analyzed by means of the stochastic math model, Markov chain.

晚二叠世晚期陆表海消亡，本区转化为内陆坳陷，形成以湖泊沉积为主的河湖充填。During the late Late Permian the epicontinental sea extincted and this area evolved into an inland depression and formed river lake fillings, mainly lake facies.

由此可见，这两类盆地的地质特征和含油气性有明显区别。The differences of geological characteristics and hydrocarbon potentials between the epicontinental foreland basin and intracontinental foreland basin are obvious.

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默兹河蜥必须呼唤空气生存，白垩纪后期浅浅的陆缘海随处可见，默兹河蜥已经很好地适应了这种环境，成为十分强劲的游泳能手。Mosasaurs breathed air and were powerful swimmers that were well-adapted to living in the warm, shallow epicontinental seas prevalent during the Late Cretaceous Period.

华北晚古生代内陆表海大型聚煤盆地的极平坦的地势是煤聚积的良好场所，而事件性海侵为泥岩沼泽发育及泥炭迅速得以保存最终形成煤层提供了条件。The extremely gentle slope of the large coal-accumulating basins in the Late Palaeozoic epicontinental seas in North China is believed to be good sites of coal accumulation.

赣西北地区下二叠统王家铺煤组和上二叠统乐平煤组，形成于陆缘海的湖泊沼泽环境。The Lower Permian Wangjiapu coal measures and the Upper Permian Leping coal measures in Northwest Jiangxi were formed in lacustrine environment in the epicontinental sea area.

马超营一一潘河大断裂，界定了古生代时期华北板块活动大陆边缘陆架与陆缘表海的南部边沿。The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.

豫西石炭系铝土矿形成于华北古夷平面上，沉积于华北陆表海-湖泊环境中。The Carboniferous bauxite deposits in the western Henan Province occur on the planation paleosurface and was deposited in epicontinental seas or lakes of the North China Block.

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层序的发育特征反映了鄂尔多斯盆地在晚古生代经历了陆表海盆地的形成、发展、衰退和逐渐消亡的过程。The characteristics of sequences reflect the process of evolution of the Ordos Basin which experimented the formation, development, waning and consumption of epicontinental basin.

在晚古生代岛弧带、弧前海沟带、弧后盆地或陆缘活动带等构造环境下发育有不同的火山岩组合。Under the tectonic backgrounds of island arc belt, fore -arc trench belt, back-arc basin, and epicontinental active belt of Late Paleozoic, it has different volcanic rock characteristics.

研究区内有两类密切共生的活动陆缘型幔源侵入岩组合，它们分属拉斑系列和钙堿系列。In the study area there exist two types of closely associated active epicontinental mantle-derived intrusive assemblages, belonging to tholeiite series and calc-alkaline series respectively.