碳酸盐台地

臼齿（Molar-Tooth）灰岩是发育于中新元古代碳酸盐台地的一种特殊灰岩类型。

Molar-tooth ( MT ) limestone is a special type of limestone developed in the Meso-and Neo-proterozoic carbonate platform .

碳酸盐台地体系包括局限台地相和开阔台地相。

Restricted platform carbonate platform system including phase and open platform .

碳酸盐台地上不同期次发育的边缘相是重要的油气储集体，它们主要分布于塔中I号断裂构造带、TZ10井构造带和塔中南缘断裂构造带上，沈积厚度相对较大。

These facies have a relatively larger thickness and are mainly distributed in the No.1 faulting zone , the TZ10 structure zone and southern edge faulting zone of the Tazhong area .

湖南永顺地区早奥陶世碳酸盐台地边缘沉积

Marginal carbonate deposition of Early Ordovician in yongshun , Hunan Province

桂林泥盆纪碳酸盐台地的发育

Development of the Devonian carbonate platform in guilin , Guangxi

布曲期为广海碳酸盐台地环境；

In Middle Buqu period , there was an open sea carbonate plateau .

桂林泥盆纪碳酸盐台地礁组合的层序地层研究

Sequence stratigraphy of Devonian carbonate platform and reef complex in Guilin , Guangxi

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 .

对于铅&锌矿产至关重要的是断陷滞流盆地相及碳酸盐台地相。

The down-faultedstagnant basin facies and carbonate platform facies have close relationship withlead and zinc deposits .

南京&巢县一带震旦纪灯影期碳酸盐台地沉积特征

The depositional characteristics of the carbonate platform of the Dengying age of Late Sinian , Nanjing-Chaoxian region

中下扬子碳酸盐台地边缘生物礁顶上。

On the top of reefs which were built up along the margin of Middle-Lower Yangtze platform .

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 .

1生物礁主要分布于晚二叠世碳酸盐台地内部和台地边缘，可分为三种类型。

The reefs are mainly distributed in the margin and the inner of the Upper Permian Changxing platform .

新疆西昆仑地区塔木-卡兰古铅锌矿带位于塔里木板块西南缘晚古生代碳酸盐台地环境中。

The Tamu-Kalangu Pb-Zn belt is located in late proterozoic carbonate tableland , southwest margin of Tarim plate .

晚侏罗世索瓦早期为高盐度、高水温，相对局限浅海碳酸盐台地环境。

In the early Suowa period of Late Jurassic , the environment was a localized sea carbonate plateau .

高桥地区马五1+2亚段时期受中央古隆起的影响，属于早奥陶系陆表海碳酸盐台地蒸发潮坪相。

Influenced by the central palaeo-uplift , Gaoqiao area belongs to the Epicontinental carbonate platform evaporative tidal phase .

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 .

将已经认识的沉积相类型和这些地震相的分布特征相比较，可以确定这种地震相就是碳酸盐台地边缘相沉积体。

Compared with those well identified sedimentary facies , these seismic facies are regarded to be the platform marginal facies .

研究区自泥盆纪起一直处于被动大陆边缘持续拉张裂陷的构造环境中，导致了碳酸盐台地多次拉张解体事件。

Research area existed in a sustaining extension rifting environment of passive continental margin . Carbonate platforms were destroyed many times .

塔里木寒武、奥陶纪盆地具有典型的三分结构，即碳酸盐台地相区、斜坡&陆棚相区和盆地相区。

Tarim basin consists of three typical sections in Cambrian - Ordovician , i.e. platform , slope - shelf and 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 .

下奥陶统与寒武系相似，碳酸盐台地发育，以灰岩、白云岩为主。

The lower Ordovician is similar to Cambrian , the carbonate platform developed and the tuff and dolomite rocks are in major .

对该剖面的详细研究，有利于恢复飞仙关期川东碳酸盐台地西侧的沉积演化过程。

Studying this section in detail is favorable to the reconstruction of the sedimentary history of the western side of the carbonate platform .

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 .

古断裂活动造成了槽台相间的古地貌格局，也是碳酸盐台地演化的古构造背景。

Ancient faulting caused the palaeomorphologic pattern of platforms alternating with troughs , and were also the palaeotectonic background of Longhuo ancient platform evolution .

广西合山煤田晚二叠世合山组是在浅水碳酸盐台地背景下形成的典型的碳酸盐岩型含煤岩系，其沉积环境有滨外陆棚、生物礁、开阔台地、潮坪和泥炭沼泽等。

The Late Permian Heshan Formation in the Heshan coal field is a typical carbonate coal measures formed in a shallow water carbonate platform setting .

三角洲砂体，浊积砂体，扇三角洲砂体，深切河谷内的河道砂体，碳酸盐台地及其斜坡脚的塌积岩是有利的储集岩体。

The deltic sand body , turbidites and fan delta sands , river channel sands . Carbonate platform and its collapsed materials are favorable reservoir .

它们在横向上的相变和垂向层序上的组合特征显示了一种发育于碳酸盐台地之上的断陷盆地的特点。

Their facies-change and the sedimentary sequences in lateral and in vertical show the character of the fault basin developed on a carbonate platform respectively .

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 .

贵州西部晚二叠世煤田位于川滇古陆和川黔碳酸盐台地之间，是颇为典型的近海煤田。

The late Permian coal fields in Western Guizhou are situated between Chuan-Dian ( Sichuan-Yunnan ) Old Land and Chuan-Qian ( Sichuan-Guizhou ) carbonate platform .