恢复了本区海西早期的岩溶古地貌。
And karst topography of this region in early Hercynian is recovered.
古地貌特征决定了层间岩溶作用的发育程度。
The ancient landform characteristic has decided the growth degree of the interlayer karst process.
因此研究古岩溶分布规律，应先进行古地貌恢复。
The study of ancient karst distribution laws should be carried out to restore the ancient landscape.
总体来说沉积相的展布受区域构造古地貌等因素控制。
General distribution of sedimentary facies by the regional tectonic control of the ancient topography and other factors.
湖相沉积主要由物源、气候和区域的古地貌特征共同决定。
Provenance, climate and the feature of palaeogeomorphology combined to effect the lacustrine sedimentation.
扇三角洲砂体的沉积特征与碎屑供应、古地貌和沉积环境密切相关。
Character of fan delta sand body is confined by sediments resource, sedimentary landform, and sedimentary environment, etc.
受潜水面阶段性上浮，相对高的古地貌上发育多期次岩溶洞穴系统。
Phased by diving surface rise, relatively high paleogeomorphology developed karst cave system in many times.
当物源和区域古地貌特征相对稳定时，气候是湖相沉积的主控因素。
When the provenance and palaeogeomorphology are pediocratic, the climate become the main factor.
在平面上受下切河谷、坡折带和地层上超尖灭等古地貌格局的制约。
The lateral distribution is controlled by palaeogromorphology including erosional valley, slope break on the …
该类储层受岩性、沉积相带、古地貌形态、成岩作用改造等因素控制。
Such reservoirs subjected to lithology, sedimentary facies belt, palaeogeomorphology, and diagenesis.
古地貌、古物源、古水动力、古基准面共同控制了滩坝砂体的形成和分布；
Palaeogeomorphology, Palaeosource, Palaeohydropower and Palaeobasal-level controls forming and distribution of beach bar sand-body.
近年来，从古地貌-沉积组合与油藏关系的角度进行油气远景评价成为研究热点。
In recent years, the evaluation of petroleum prospective has become a hot research topic from the aspect of the relationship between the ancient landform-sedimentary assemblage and the oil reservoir.
分流河道和席状砂为有利储层，砂体展布形态主要受控于物源远近及古地貌形态。
Channel and Sheet sand are sweet reservoir. Distribution of sand is controlled by provenance distance and palaeogeomorphology.
构造活动主要通过对沉积古地貌的控制而控制着沉积物的分布及沉积物本身的特征。
Structure activity controlled the distribution and characteristics of sediments by controlling the palaeogeomorphology of sedimentation.
采用回归法分析了矿体厚度与古地貌之间的关系，据统计研究，矿体厚度属随机变量。
Correlation factors between them are analyzed via statistic regression, where thickness of ore formation is regarded as a random variation.
古隆起的东南和东北缘发育的主要同沉积断裂形成明显的古地貌突变带或断裂坡折带。
The main syndepositional faults along the southeastern and northeastern margins of the ancient uplift formed obvious geo-morphologic abrupt zones or fault slope-break zones.
古地貌形态、断裂活动期次、强度及坡折带的发育控制了扇体的数量、规模与迁移方向。
It is pointed out that, the number, scale and migration direction of fans were controlled by palaeogeomorphology, periods and strength of fault movement, and the development of slope-bend belt.
古岩溶发育受多种因素影响，其中古地貌形态是控制古岩溶发育及分布的主要因素之一。
Ancient karst development is affected by multiple factors, the ancient landscape is one of the major factors to control development and distribution of the ancient karst.
通过对区域应力场、古地貌和断裂空间展布等分析，认为垦东地区发育“隐伏型”走滑断裂。
Through the analysis on stress field, palaeogeomorphology and spatial distribution of faults, Kendong region is considered to be 'concealed' strike - slip fault.
因此古地貌高地、古地貌斜坡与洼地中的局部地貌隆起将是层间岩溶作用发育的最有利区带。
Therefore the partial landform uplift among the ancient landform highland, the ancient landform slope and the marsh land will be most advantageous area belt of the growth of interlayer karst process.
构造运动造就的古地貌在陆相盆地，特别是裂谷盆地对层序形成与发育起着重要的控制作用。
Paleo morphology resulted from tectonic movement controlled the sequence formation and development of continental basins, especially of rift basins.
鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。
The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.
在层序地层体制中，储层的纵向发育受基准面升降变化旋回的控制，而平面展布受古地貌的制约。
In sequence stratigraphic system, vertical development of the reservoir is controlled by base level cycle changes, and spatial distribution is restricted by the palaeogeomorphology.
孤北断层持续不均衡发育形成孤北斜坡带沟梁相间、陡缓变化的古地貌，古地貌控制了隐蔽圈闭的平面分布。
Continuous disproportionate growth of Gubei fault formed the palaeogeomorphology of Gubei slope belt with groove alternating with roof and with abrupt and gentle change.
进一步分析，这些沉降中心的形成明显受到了周缘山系逆冲推覆作用的构造负载和盆地基底构造的制约，使盆地形成了隆坳相间的古地貌格局。
The formation of these quick subsidence centers were obviously controlled by the tectonic load derived from the adjacent orogenic thrusting and preexisting tectonic blocks in the basin basement.
因此，精细恢复古地貌形态，建立地质储层模型，研究古地貌油气富集规律，对于整个鄂尔多斯盆地的侏罗系油气勘探工作具有十分重要的意义。
So it is important to rebuildpalaeogeomorphology and geology reservoir model and study oil-gas accumulationregulation accurately for oil-gas exploration of Jurassic in Ordos Basin.
现代松辽水系是在松辽盆地地质构造、古地貌发育的基础上，几经变迁逐渐演变而成的。晚第三纪以来，古松辽水系经历了几次大规模的河湖交替。
Since the Neogene, the ancient Songhua-Liao River system have undergone several changes with the alternation of fluvial and lacustrine formation on a large scale.
同时位在表面的无人探测车精神号和机会号，继续检视火星的地貌、岩石和土壤，寻找火星古水世界存在的线索。
Meanwhile, down on the surface, robots Spirit and Opportunity continue to roll, inspecting landscape, rocks, and soil for clues to the ancient watery past of the red planet.
据堆积过程，把自然泥石流堆积地貌分为古泥石流台地、老泥石流台地和近代泥石流长柄扇。
According to the genesis, the accumulational landform of debris flow may be classified into natural and man-made ones.
据堆积过程，把自然泥石流堆积地貌分为古泥石流台地、老泥石流台地和近代泥石流长柄扇。
According to the genesis, the accumulational landform of debris flow may be classified into natural and man-made ones.
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