• The carbonate platform sedimentary system is further divided into such facies as restricted platform, open platform, platform margin reef and ramp.

    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。

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  • The both sides are carbonate platform, while the middle part shows a deepwater interplatform basin.

    两侧为碳酸盐台地,中间为深水台盆。

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  • Only the limestone of the middle limestone member may deposit in shallow sea carbonate platform environment.

    唯有本部灰岩段可能属于浅海碳酸盐岩台地沉积。

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  • Nodular limestone was formed in the shallow-water zone in the carbonate platform, and the water was turbid with mud.

    瘤状灰岩形成于碳酸盐台地浅水部位,水体为半浑浊。

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  • The reef oil-gas pool in the carbonate platform of Dongsha Massif is one of the most important exploration directions.

    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。

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  • The drowning of the carbonate platform is one of the most spectacular geological processes in the Late Ordovician on Yangtze block.

    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。

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  • The Feixianguan Formation of evaporative carbonate platform is a set of sulfate-bearing evaporative tidal sediments with aboundant dolomite.

    飞仙关组蒸发台地为一套含硫酸盐的富白云岩的蒸发潮坪沉积层系。

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  • The Permian organic reefs, most of them belong to sponge reefs, which are widely developed in the carbonate platform areas of the South China.

    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。

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  • The sedimentary facies of Carboniferous Bioclastic Limestone Member is mainly classified into shore and carbonate platform facies in Tarim basin.

    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。

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  • Abstract: As the transition zone between terrestrial and Marine environment, carbonate platform sediments record information both from ocean and land.

    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。

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  • 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.

    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。

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  • The drowning event is a key marker representing the termination of carbonate platform development and has some features of geology, geochemistry and seismic reflection.

    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。

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  • 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.

    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。

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  • 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.

    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。

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  • The oolite beach of the lower Triassic Feixianguan Formation in eastern Sichuan basin developed in themargin of carbonate platform, and platform margins are always related to ocean trough.

    四川盆地东部下三叠统飞仙关组鲕滩主要发育在碳酸盐岩台缘带上,而台缘带与海槽密切相关,找到了海槽就意味着找到了鲕滩。

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  • The oolite beach of the lower Triassic Feixianguan Formation in eastern Sichuan basin developed in themargin of carbonate platform, and platform margins are always related to ocean trough.

    四川盆地东部下三叠统飞仙关组鲕滩主要发育在碳酸盐岩台缘带上,而台缘带与海槽密切相关,找到了海槽就意味着找到了鲕滩。

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