陆表海 meaning in Chinese
continental sea
eperic sea
Examples
- In the taiyuan stage of the early permian , north china sea is connected with qilian sea to form uniform epicontinental sea deposit
早二叠世太原期，华北海与祁连海贯通，形成统一陆表海沉积阶段。 - Started from benxi stage of late carboniferous , deposits of epiric sea were developed in this area along with the spreading of west - east direction and gentle depression of the basement
从晚石炭世本溪期开始，由于东西向拉张，基底缓慢下沉，本区广泛发育陆表海沉积。 - Calculation of transition probability matrix and fixed vector of the well profiles in the area shows , from a quantitative point of view , the vertical evolution law of the sedimentary series and the transversal environmental difference
通过多步转移概率矩阵和固定向量计算，从定量的角度说明了研究区内部分钻井剖面陆表海沉积在垂向上演化的规律性及反映在横向上的古环境差异性。 - It is considered that the sequence evolution in the palaeozoic went through the following three stages , the filling of evaporate platform , the filling of carbonate and detrital rock mixed deposits in epiric sea , and the filling of detrital deposits of lake - deltas in paralic inland sag
认为研宄区古生界层序演化经历了以下三个阶段：蒸发台地充填阶段、陆表海碳酸盐岩与碎屑岩混合沉积阶段，以及近岸内陆坳陷的湖泊三角洲碎屑岩沉积阶段。 - According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。