两侧为碳酸盐台地，中间为深水台盆。
The both sides are carbonate platform, while the middle part shows a deepwater interplatform 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.
它的基本环境模式是碳酸盐台地与台后盆地。
The carbonate plateform and back-plateform basin are the basic environmental model of the Chartai Group.
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.
野云沟组主要为斜坡相和盆地相沉积，少量为碳酸盐台地相沉积。
Yeyungou Formation mainly developed carbonate slope facies, deep water basin facies and a little carbonate open platform facies.
研究区的生物礁为碳酸盐台地边缘缓坡点礁群，沿着台地边缘断续分布。
Organic reefs in the study region form a patch reef group on the carbonate platform margin ramp and they are interruptedly distributed along the platform margin.
滇西保山—施甸地区泥盆系沉积相类型包括碳酸盐台地相、陆棚相反盆地相。
The sedimentary facies type of Devonian in Baoshan-Shidian district consists of carbonate platform, shelf, slope and basin facies.
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.
广西泥盆纪的沉积相可划分为滨岸碎屑岩相、碳酸盐台地相和陆间海槽相等三个相区。
Study on the Devonian sedimentary facies in Guangxi reveals that it may be plotted to three facies areas: shoreface clastic area, carbonate platform area and inter-land sea trough.
碳酸盐台地沉积体系又可进一步分为局限台地、开阔台地、台地边缘礁滩及缓坡等沉积相。
The carbonate platform sedimentary system is further divided into such facies as restricted platform, open platform, platform margin reef and ramp.
东达村组自下而上为冲积扇泥石流沉积、无障壁碎屑滨岸沉积和浅水碳酸盐台地潮坪沉积。
The Dongdacun Formation consists in ascending order of alluvial fan debris flow deposits, barrier-free clastic littoral deposits and shallow-water carbonate platform tidal-flat deposits.
根据沉积相的空间展布，隆或古台地在石炭纪时为一个孤立的碳酸盐台地，周围被海槽围限。
According to space distribution of the sedimentary facies, Longhuo ancient platform was an isolated one, surrounded with troughs in the Carboniferous period.
通过对该地层中岩石特征及沉积环境等方面的分析，认为该区在研究层段内属于碳酸盐台地相。
According to the analysis of rocks features and sedimentary environment, the section pertains to carbonate tableland 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;
碳酸盐台地高水位溢流是指在海平面高水位期，台地沉积物被搬运到斜坡及较深水盆地中沉积下来所形成的沉积体。
The term "highstand shedding of carbonate platforms" means that carbonate plat forms shed most their sediments into the slopes or the formed sediments deposit into the deeper basins.
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.
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.
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.
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.
在川东北地区演化为碳酸盐蒸发台地。
The northeastern Sichuan area is evaporative carbonate platform.
碳酸盐的沉积环境主要为台地相。
The sedimentary environment of carbonate is platform facies.
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.
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.
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.
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.
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.
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.
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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