Weibei basin is a Mesozoic-Cenozoic basin developed in the Tanlu fault zone.
潍北盆地是发育于郯庐断裂带内的中、新生代盆地。
Urxun-Beier depression in Hailaer Basin is the Mesozoic-Cenozoic basin located in the Paleozoic orogenic belt in Inner Mongolia-Daxing'anling area.
海拉尔盆地乌尔逊-贝尔凹陷是叠置于内蒙-大兴安岭古生代碰撞造山带的中新生代盆地。
Northeast Sichuan basin is a Mesozoic-Cenozoic basin in north margin of the Yangtse plate, which has a complex tectonic background and hydrocarbon accumulation history.
川东北地区是上扬子板块北缘的中新生代含油气盆地，具有复杂的构造和成藏历史。
Abstract1 Northeast Sichuan basin is a Mesozoic-Cenozoic basin with complex tectonics, Triassic formation based on Marine deposits was an important potential resource and reservoir.
川东北地区是一个具有复杂构造的中新生代盆地，以海相沉积为主的三叠系是重要的储层。
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.
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。
Liaohe basin is a rift basin developed in the Mesozoic and Cenozoic.
辽河盆地是中、新生代发育起来的裂谷盆地。
The Southern Huanghai (Yellow) Sea is a part of the North China platform and Yangtze platform, and is a large Mesozoic and Cenozoic composite basin consisting of uplifts and depressions.
南黄海属于华北地台及扬子准地台的一部分，是一个由隆起、拗陷组成的中、新生代大型复式盆地。
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、地质等资料，结合野外地质及前人研究成果，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。
The strata of Mesozoic and Cenozoic in the basin can be divided into three parts, Middle Jurassic (Longjiagou Formation ), Lower Cretaceous and Upper Miocene (Baode Formation ).
根据化石组合，龙家沟盆地的地层可划分为中侏罗统龙家沟组，上白垩统及上中新统保德组。
Erlian basin, a cluster of rift lake basins in the Mesozoic and Cenozoic eras developed on the base of the Hercynian fold belt, consists of 50 sags in different scale.
二连盆地是在海面褶皱基底上发育起来的中新生代断陷湖盆群，共发育大小不等的50个凹陷。
The characteristics of structure and depositment in this Mesozoic and Cenozoic time show that Bohai basin is a Mesozoic and Cenozoic composite basin.
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。
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.
到晚白垩世至古新世则为盆地挤压隆升剥蚀期，形成了中-新生界之间较大的角度不整合。
Kaping Jianhe region situated in the boundaries of Tangshan City is a basin superposed by Paleozoic, Mesozoic and Cenozoic sediments.
开平涧河地区位于河北省唐山市境内，是一个由古生界、中生界及新生界叠合而成的构造盆地。
Chuxiong basin is a typical reformed basin, which formed during Mesozoic-Cenozoic periods in south of China and has good petroleum geological condition.
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。
Bohaiwan basin is a composite basin polymerized by a Mesozoic and Cenozoic rift basin and a Carboniferous remnant coal-bearing basin.
渤海湾盆地是中、新生代裂谷盆地与石炭-二叠系残留含煤盆地的复合叠合盆地。
Shiwanshan basin has a Mesozoic to Cenozoic continental sedimentary cover lies over a basement of marine-facies Indosinian deformation.
十万山盆地是在印支期海相沉积基底上发育的中新生界陆相沉积盆地。
Yuzhong Basin is located in the middle part of Lanzhou Dingxi Mesozoic Cenozoic depression.
榆中盆地位于兰州—定西中新生代凹陷盆地的中部。
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.
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。
Huahai sag is a small sedimentary fault-depression basin formed during Mesozoic-Cenozoic periods, its accumulation conditions of oil and gas represent the characteristics of medium-small basins.
花海凹陷是一个小型的中新生代沉积断陷，其油气成藏条件在中小型盆地中具有代表性。
Miyang Depression is a Mesozoic-Cenozoic fault basin, where lithologic change is fast, fault is developed, reservoir type is various.
泌阳凹陷是一个中新生代断陷盆地，岩性变化快，断裂发育，油藏类型多。
Durimu sag is a Mesozoic Cenozoic sag of Erlian Basin and its landscape is a part of Tengger Desert.
都日木断陷是二连盆地中一个中新生代单断型凹陷，其地表景观为腾格尔沙漠的一部分。
The tectonic dynamic setting in the south border of Junggar Basin has been generally considered as a Mesozoic- Cenozoic compressive basin.
准噶尔盆地南缘在中生代、甚至新生代很长一段时间处于拉张伸展环境。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
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