• Fault analysis show that Taiyuan basin is sedimentary basin of Late Cenozoic rather than rifted one.

    断裂分析太原盆地不是裂谷盆地,而是新生代沉积盆地。

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  • The fourth phase is that the NS graben structure was produced by EW expanding mechanism in late Cenozoic.

    第四变形新生代晚期东西向伸展机制产生南北向地堑构造

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  • There are at least nine physiographic cycles in the middle reaches of the Yellow River during the Late Cenozoic Era.

    新生代黄河中游至少存在九个地文期旋回。

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  • The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.

    准噶尔盆地南缘的新生代构造变形认为是天山地区印度欧亚板块碰撞与会聚作用过程的构造响应

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  • Konggur in Late Cenozoic; the inflexion of every elevation rise gradient may be the dividing point of different uplift process.

    每个抬升梯度拐点,则对应着不同隆升过程形成海拔高度分界点

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  • The Yecheng foreland basin is a part of the southwest sag of the Tarim Basin and contains late Cenozoic molassic deposits with great thickness.

    叶城盆地属于塔里木盆地西南坳陷,在新生代沉积了巨的磨拉石建造。

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  • There occur thick wind-blown silt deposits which are regarded as a good geological archive of paleoclimatic changes in Late Cenozoic in North China and the central Asia.

    中国北方连续堆积新生代风成红粘土-黄土,气候干湿变化的良好地质记录

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  • A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.

    通过东大滩—东温泉地区的路线地质观测与构造填图昆仑南部发现新生代大型逆冲推覆构造系统

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  • The sediments of the late Cenozoic in the Jiuxi basin, located in the northern margin of the Tibetan plateau, have sensitively and completely recorded the uplifting process of northern plateau.

    位于青藏高原北缘西盆地新生代沉积比较敏感全面记录高原北部构造运动和隆升过程

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  • The late Cenozoic geomorphologic and sedimentary features in the west Kunlun Mountain front record the uplift process of the west Kunlun Mountains and the western margin of the Qinghai-Tibet Plateau.

    西昆仑山前晚新生代地貌沉积特征记录西昆仑山青藏高原西北缘隆升过程

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  • In the southern North China, the lower Paleozoic source rocks reached primary maturation at late Triassic and the secondary hydrocarbon generation did not occur at the Cenozoic.

    华北地区古生界烃三叠世达到早成熟阶段,新生代基本发生二次生作用。

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  • The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.

    中国古生代中生代新生代大地构造性质各个地区不同。

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  • The following examples of oil and gas fields in distributary and delta- fringe sand bodies range in age from late paleozoic to middle cenozoic.

    下面列举是分布分流三角洲前绿油气田的例子,地质时代古生代至中新生代。

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  • It was rift basin in Late Jurassic Early Creaceous and squeezed sag basin since Cenozoic.

    侏罗纪白垩世为拉张断盆地第三纪以来挤压陷盆地。

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  • The structural characteristic of the North Ordos basin in the Late Mesozoic and the Cenozoic is researched with the data of seismic, geological and former achievements.

    根据地震地质资料,结合野外地质前人研究成果,对鄂尔多斯盆地北部中生代晚期以来后期改造特征进行了研究。

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  • The salt-related tectonics in the Qiangtang basin mainly formed in late Jurassic and was further patterned during Cenozoic.

    羌塘盆地盐相关构造形成侏罗纪新生代进一步定型

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  • Basin evolution in ne China goes through four stages: early Jurassic rift basin, middle-late Jurassic partitioned foreland basin, late late Jurassic-Cretaceous rift basin and Cenozoic rift basin.

    东北地区新生代盆地演化经历侏罗世陷盆地、中晚侏罗世分割式前陆盆地、侏罗世末期至白垩纪裂谷盆地新生代裂谷盆地四个演化阶段

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  • Generally, the basin is a superimposed basin formed by foreland depression of the Late Paleozoic in the lower, and the piedmont depression of the Meso-Cenozoic in the upper.

    古生代坳陷中新生代山前拗加而成复合型盆地

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  • From late Cretaceous to Paleocene, it is the time of basin extruding, uplifting and denudation, therefore a larger angular unconformity formed between Mesozoic and Cenozoic.

    白垩古新世盆地挤压隆升剥蚀形成了中-新生界之间较大角度不整合

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  • The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.

    矿山梁构造几何学上表现个双重构造:浅层是一个世形成断层转折褶皱深层则是在新生代形成三个冲岩叠置所构成的隐伏堆垛背斜构造。

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  • Thus we suggest that the Late Palaeozoic sediments are not the metamorphosed basement in the Mesozoic-Cenozoic basins, they are superimposed basins.

    因此古生不是松辽盆地和二连盆地变质结晶基底它们一种叠合盆地关系。

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  • Thus we suggest that the Late Palaeozoic sediments are not the metamorphosed basement in the Mesozoic-Cenozoic basins, they are superimposed basins.

    因此古生不是松辽盆地和二连盆地变质结晶基底它们一种叠合盆地关系。

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