南京附近的古砾石层是组成该区新生代地层重要岩石类型之一。
The ancient gravel beds in the suburbs of Nanjng is one of the important types of rock of the Cenozoic era.
因此，这里提出的沉降分析被截断在连续的新生代地层剖面顶部。
Therefore, the subsidence analysis presented here is truncated at the top of the continuous Cenozoic stratigraphic section.
井的测试结果与储层分析都证明前新生代地层有良好的储集性能。
Core test and reservoir analysis show that there exists certain good reservoir in the Pre Cenozoic stratum.
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.
新生代地层中砾岩砾石成分稳定，以变质岩和沉积岩成分居多，岩浆岩很少；
Gravels components from the Cenozoic strata are mainly composed of metamorphic rocks and sedimentary rocks with little magmatic rocks.
区内新构造运动迹象明显，在地貌、新生代地层变形、断裂新活动等方面均有反映。
The sign of neotectonism in this area is obvious, which is reflected in land form, formation deformation in new born zone, new movement of fault, etc.
依据中国海域地层研究资料，论述了中国海域的前中生代地层和中、新生代地层的研究现状。
On the basis of research data about strata in China sea areas, the current situation of study on pre-Mesozoic, Mesozoic and Cenozoic strata in the sea areas are expounded.
通过共和盆地西北部晚新生代地层的野外地质调查，发现上新世地层中存在一期角度不整合面。
An angular unconformity within the Pliocene stratum was found during field exploration in northwestern part of the Gonghe Basin.
南京附近的古砾石层是该地区新生代重要地层之一。
Paleogravel bed around Nanjing city is one of primary Cenozoic strata in Nanjing area.
辽宁省中新生代盆地地层中赋有有丰富的地热资源。
Rich geothermal resources are hosted in the Meso-Cenozoic basins in Liaoning Province.
新生代火成岩分布于下第三系地层中，为基性的喷发岩或侵入岩，由南向北，时代变新，厚度及分布范围增大。
In the Jizhong Depression, the Cenozoic igneous rocks, distributing within the Eogene strata, trend to be younger in age but increase in thickness, and in area from the south toward the north.
从海参1井钻井剖面出发，建立六盘山盆地中新生代层序地层格架。
Starting from the profile of Haishen no. 1 well, this paper establishes the sequential stratigraphic framework of middle Cenozoic in Liupanshan Basin.
通过深入揭示残留地层所蕴涵的构造信息，为正确认识渤海湾盆地新生代形成演化机制提供了新的依据。
Through deep revealment of the geological information, new evidence was obtained for a correct recognition of the Cenozoic forming and evolution mechanism of Bohai Bay Basin.
通过深入揭示残留地层所蕴涵的构造信息，为正确认识渤海湾盆地新生代形成演化机制提供了新的依据。
Through deep revealment of the geological information, new evidence was obtained for a correct recognition of the Cenozoic forming and evolution mechanism of Bohai Bay Basin.
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