撞击表明了前新生代盆地的结构，残余厚度和地下三分性。
Pre-Cenozoic basin structure, residual thickness and trichotomous property of basement are all shown by the impact.
从渤海湾盆地的中、新生代构造演化分析，渤海湾盆地是一个新生代早第三纪始新世形成的走滑拉分盆地。
According to the analysis of Mesozoic and Cenozoic tectonic evolution, Bohai Bay basin is a strike slip pull apart basin formed in the Cenozoic Eocene epoch.
辽河盆地东部凹陷北段新生代盆地具下断上拗的双层结构，是伸展和走滑联合作用的断陷盆地。
Cenozoic East Sag of Liaohe basin consists of double structure and is a fault depression basin with extending and strike slipping.
具有工业意义的油气田均位于构造隐性急变带与中新生代盆地的立交地段。
The most of oil fields with industrial index are also located at the cross districts between basin and tectonic recessive geochemical boundaries.
辽河盆地是中、新生代发育起来的裂谷盆地。
Liaohe basin is a rift basin developed in the Mesozoic and Cenozoic.
山西太原盆地是我国北方典型的大型新生代断陷盆地。
Taiyuan basin is a representative large-scale Cenozoic rift basin in Shanxi Province, northern China.
根据铀矿床的形成机制，对滇西地区新生代盆地的砂岩型铀矿成矿模式进行了探讨。
A genetic model for the sandstone type uranium deposits in Cenozoic basins of western Yunnan is proposed.
新生代裂陷盆地旋回又划分为早期裂陷、强烈裂陷、晚期裂陷和晚第三纪整体坳陷4个阶段。
The latter can be subdivided into 4 stages, including initial rifting, intense rifting, late rifting and Late Tertiary integral downwarping.
由于发育大量不同类型中生界和新生界的沉积盆地，中国大陆应赋存有大量的石油和天然气。
For there exist a lot of Mesozoic and Cenozoic depositional basins of different types, China's Mainland should be very rich in oil and gas resources.
经断裂分析，太原盆地不是裂谷盆地，而是晚新生代的沉积盆地。
Fault analysis show that Taiyuan basin is sedimentary basin of Late Cenozoic rather than rifted one.
活动性强、深部作用活跃，是中国沉积盆地，特别是中、新生代盆地的两个重要特点。
Strong activity and active deep action are two important features of Chinese sedimentary basins, especially for Meso-Cenozoic basins.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu Tancheng?
楚雄盆地是我国南方具有良好石油地质条件的大中型中-新生代改造型含油气盆地的一个典型代表。
Chuxiong basin is a typical reformed basin, which formed during Mesozoic-Cenozoic periods in south of China and has good petroleum geological condition.
新生代盆地构造和沉积分布特征表明渤海湾盆地是一个中、新生代叠合盆地。
The characteristics of structure and depositment in this Mesozoic and Cenozoic time show that Bohai basin is a Mesozoic and Cenozoic composite basin.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
万安盆地是南海重要的新生代含油气盆地之一，是较为典型的新生代走滑拉张盆地。
Wan 'an basin is one of the most important Cenozoic oil and gas basins in the South China Sea, and it is also a typical Cenozoic strike-slip extensional basin.
松辽盆地地处中国东北部是中新生代形成的大型陆相盆地，是我国重要的石油产区。
Songliao basin is a large scale land basin of Meso-cenozoic at northeast of China, which is one of the most important oil-producing area.
潍北盆地是发育于郯庐断裂带内的中、新生代盆地。
Weibei basin is a Mesozoic-Cenozoic basin developed in the Tanlu fault zone.
迈卢特盆地是苏丹东南部中—新生代的一个大型陆内裂谷盆地。
Melut Basin is a large-scale basin of the Cretaceous-Paleogene sediment in the southeastern Sudan.
根据胶莱盆地区域地质特征，地球动力学背景及盆地中、新生代沉积特征分析，论述盆地的发育和演化阶段，并对胶莱盆地含油气前景进行探讨。
The evolution features of the Jiaolai Basin are discussed in this paper on the basis of its regional structure, geodynamic background and sedimentary features of the Mesozoic and Cenozoic.
在快速沉降的新生代盆地，由于泥岩快速生油而又难以排放，形成局部异常高压带。
Local abnormal high pressure zones are formed in swift burial Cenozoic basins because mudstone generates oil quickly and releases with difficulty.
塔西南前陆盆地是古生代克拉通盆地与中、新生代前陆盆地的复合，在剖面上呈向北抬升的箕状结构。
The southwest foreland basins in Tarim Basin is composed of Paleozoic basins and the Meso Cenozoic foreland basins.
榆中盆地位于兰州—定西中新生代凹陷盆地的中部。
Yuzhong Basin is located in the middle part of Lanzhou Dingxi Mesozoic Cenozoic depression.
古生界烃源岩在新生代盆地沉降期间“二次生烃”，生成的天然气通过断裂向上运移至第三系储集。
In the subsidence period of the Cenozoic basin, the hydrocarbons generated secondarily by Palaeozoic source rocks migrated upward and passed through fault to Tertiary reservoir.
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.
中国东、南部沿着一些深大断裂带分布有140多个中、新生代残留型小盆地。
There are more than 140 minor Meso-Cenozoic remnant basins distributed along deep fault zones in south-east China.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
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