唯有本部灰岩段可能属于浅海碳酸盐岩台地沉积。
Only the limestone of the middle limestone member may deposit in shallow sea carbonate platform environment.
碳酸盐岩台地广泛发育及其淹没事件是南海新生代地层的重要特征之一。
Development of Cenozoic carbonate platforms is one of the most spectacular stratigraphic features in the South China Sea.
碳酸盐岩台地广泛发育及其淹没事件是扬子地区晚奥陶世地层的重要特征之一。
The drowning of the carbonate platform is one of the most spectacular geological processes in the Late Ordovician on Yangtze block.
广泛发育于我国南方碳酸盐岩台地区的二叠纪生物礁，其中绝大多数属于海绵生物礁。
The Permian organic reefs, most of them belong to sponge reefs, which are widely developed in the carbonate platform areas of the South China.
摘要：碳酸盐岩台地作为陆地与深海间的过渡带，其沉积记录了海洋和邻近陆地的演化。
Abstract: As the transition zone between terrestrial and Marine environment, carbonate platform sediments record information both from ocean and land.
东沙隆起碳酸盐岩台地生物礁、滩油藏的勘探，是珠江口盆地（东部）重要的勘探领域之一。
The reef oil-gas pool in the carbonate platform of Dongsha Massif is one of the most important exploration directions.
川东北地区罗家寨飞仙关组鲕滩储集层为碳酸盐岩台地边缘相沉积，具有厚度大、分布稳定的特点。
Oolite beach carbonate reservoir of Feixianguan Formation in Luojiazhai, NW Sichuan Basin is a platform edge facies sediment with massive thickness and uniform distribution.
沉没事件是碳酸盐岩台地发育、演化终止的一个重要标志，它具有特定的地质、地球化学及地震反射特征。
The drowning event is a key marker representing the termination of carbonate platform development and has some features of geology, geochemistry and seismic reflection.
深入研究了塔里木盆地北部奥陶系中部一段台地—盆地相序列中的高分辨率碳酸盐岩旋回的特征。
The characteristics of high resolution carbonate cycles in a sequence composed of platform and basin in the middle part of Ordovician in the North Tarim basin have been studied.
湘南泥盆系碳酸盐岩的沉积环境，可以区别为四种类型：台地相、广海陆棚相、生物礁相及台盆相。
The sedimentary environments of the Devonian carbonate formations in southern Hunan, China can be divided into four types: platform, open marine shelf, bioherm, and platformbasin facies.
通过野外观察，微生物岩出露的古地理位置大致可以分为三类：（1）南盘江盆地内孤立碳酸盐台地上；
The microbialites' paleogeography position can be divided into three types: (1) on the top of the isolated carbonate platform within the Nanpanjiang Basin;
石头山灰岩为浅海碳酸盐台地稳定沉积；
The Shitoushan Limestones are assigned to the stable deposits on shallow-marine carbonate platforms.
塔里木盆地石炭系生屑灰岩段的主要沉积相类型划分为滨岸相和碳酸盐台地相两大类。
The sedimentary facies of Carboniferous Bioclastic Limestone Member is mainly classified into shore and carbonate platform facies in Tarim basin.
瘤状灰岩形成于碳酸盐台地浅水部位，水体为半浑浊。
Nodular limestone was formed in the shallow-water zone in the carbonate platform, and the water was turbid with mud.
结果表明，震旦系-下古生界(下组合)主要为一套浅海陆棚相碎屑岩与台地相碳酸盐岩沉积序列。
The results indicate that there mainly develop a set of shallow Marine shelf clastic sedimentary rocks and platform carbonate rocks during the Sinian-Lower Paleozoic (Lower Assemblage) period.
陡山沱组盖帽碳酸盐岩形成于温暖条件下、微咸化海水沉积环境，属潮间—潮下台地前缘斜坡和浅海盆地之间的过渡带。
The precipitation of Doushantuo cap carbonates was deposited in warm, brackish water, and between the intertidal-subtidal inner ramp and shallow basin.
陡山沱组盖帽碳酸盐岩形成于温暖条件下、微咸化海水沉积环境，属潮间—潮下台地前缘斜坡和浅海盆地之间的过渡带。
The precipitation of Doushantuo cap carbonates was deposited in warm, brackish water, and between the intertidal-subtidal inner ramp and shallow basin.
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