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  • Continental faulted basins formed in specific depositional environment.

    陆相断陷盆地具有特定的沉积环境。

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  • Faunal assemblage are directly related to the depositional environment.

    动物群落与沉积环境有直接关系。

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  • There were obvious depositional response in the extensional faulted basin.

    在伸展断陷盆地内均有明显的沉积响应。

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  • There exited many types of the depositional gap within depositional sequence.

    在古河谷沉积层序中存在着多种沉积间断。

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  • Depositional base-level cycle controls the development and evolution of sequence stratigraphy.

    沉积基准面旋回变化控制着陆相层序地层的形成与演化。

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  • Braided delta and lacustrine facies are two major depositional systems developed in Liushagang Fm.

    流沙港组主要发育辫状河三角洲相和湖泊相两种沉积体系。

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  • The subaqueous Changjiang River delta has its own distinctive depositional processes and products.

    长江水下三角洲是一个以径、潮流相互作用为主的沉积体。

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  • Using the special influence of the structure on the pressure, depositional uncontinuity is analyzed.

    还利用构造对压力产生特殊影响,分析了沉积的非连续性等。

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  • By analyses, the main reason of poor reservoir heterogeneity is the change of depositional environment.

    综合分析认为,引起储层非均质性的主要原因是沉积环境的变化。

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  • Changes in depositional base-level cycle control the development and evolution of sequence stratigraphy.

    沉积基准面旋回变化控制着陆相层序地层的形成与演化。

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  • The hydrocarbon generation, migration and accumulation are strongly controlled by depositional features.

    油气的生成、运移与聚集都受沉积特征的强烈控制。

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  • The thin-beded siliceous -rocks include chert and depositional quartz with textures of oolite and pebble.

    矽质岩包括燧石和沈积石英岩,呈薄层状产出,沈积石英岩具鲕状、砾状结构。

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  • These beds are the direct evidence for the occurrence of the Neogene lacustrine depositional environment.

    这是渤海新近纪湖相沉积地层存在的直接证据。

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  • The crystalline temperature and the hardness of the amorphous electro-depositional coating were determined.

    对非晶合金电沉积镀层的晶化温度和硬度进行了测定。

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  • It looks like depositional rocks. There is a fault and the calcite nodule are precipitated after the faulting.

    看起来像是沉积岩。有断层存在,在发生断裂后有方解石脉沉积。

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  • Different types of depositional basin held different structure styles and underwent different tectonic acting.

    不同盆地类型具有不同的构造格局和构造活动特征。

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  • The depositional slope-break belt controls the development of sediment system of eroded valley-low stand delta.

    低水位时期坡折带控制了下切谷-低位三角洲沉积体系的发育。

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  • Highstand System Tract mainly develops depositional system of offshore-meare, fluvial facies and prograded delta.

    高位体系域主要发育滨浅湖相、河流相及进积型三角洲沉积体系。

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  • Black shales have been considered as a sign of anoxic depositional environments and anoxic events for a long time.

    富有机质黑色页岩的形成长期以来被认为是缺氧沉积环境的证据,并被作为全球缺氧事件的标志。

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  • For lithologic reservoirs, the width of sandstone distribution is different in different depositional environments.

    对于岩性油藏,不同沉积环境所形成砂体的展布宽度是有差异的。

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  • Depositional district: lithologically, they are sandy conglomerate, sandstone, siltstone interbedded with mudstone.

    沉积区:岩性由砂砾岩、砂岩、粉砂岩夹泥岩组成。

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  • This paper has studied the evolutionary tendency of depositional environment, sediment resource and its geomorphic forms.

    对莱州湾的沉积环境演变趋势、泥沙资源及其沉积地貌形态进行了研究。

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  • The eastern part region of Qidam basin is a Quaternary depositional and subsidence center being large and extensively distributed.

    柴达木盆地东部地区是第四纪的沉积与沉降中心,内陆湖泊相的沉积厚度大、分布广泛。

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  • There are complex and regular changes in depositional facies from the early to the middle Triassic strata in the Nanpanjiang Basin.

    南盘江盆地的早—中三叠世地层中,沉积相形成复杂而有序的空间变化和时间变化。

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  • The correlation between these sequences and the depositional sequences of the plat were given on the basis of biostratigraphic data.

    依据生物地层学资料和层序顺序,将这些层序与台地相区沉积层序逐一进行了对比。

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  • Depositional facies, a term of petroleum geology, is a combination of sedimentary rocks produced by a certain depositional environment.

    沉积相是石油地质学中的一个术语,是指一定的沉积环境所形成的沉积岩组合。

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  • The Central Livingston Island was at a special tectonic setting, fan depositional environment, during Late Palaeozoic Early Mesozoic time.

    在晚古生代至早中生代,利文斯顿岛中部处于一个独特的浊积扇的构造环境。

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  • The Central Livingston Island was at a special tectonic setting, fan depositional environment, during Late Palaeozoic Early Mesozoic time.

    在晚古生代至早中生代,利文斯顿岛中部处于一个独特的浊积扇的构造环境。

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