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.
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.
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.
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.
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.
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.
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.
泻湖是全新世海侵以来发育的以淤积为主的海岸地貌，其沉积地层蕴含了丰富的古环境演变信息。
Lagoon is the coastal landscape developed by the deposition mainly since Holocene transgression, and the stratigraphic of which contains a wealth of paleoenvironment evolution information.
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.
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.
古人类活动遗址所处地貌部位为古永定河冲积扇的河间冲积平原。
The landform on which ancient human activity relic located was interfluvial floodplain on Yongding River Alluvial Fan.
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.
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.
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.
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.
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.
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.
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.
在太白山及其邻近地区的高山带，分布着大量的古冰川地貌。
There are abundant traces of ancient glaciation distributed on the high mountain belt of the mount Tai-Bai and its near areas.
太白山是我国东部古冰川地貌保存较好的山地。
The ancient glacial remains in Taibaishan was glacial relief area, which was remained very well in the East of China.
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.
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.
由于处在古火山频繁活动的地带，山体呈现出独具特色的峰、柱、墩、洞、壁等奇岩怪石，称得上是一个造型地貌博物馆。
Because of frequent activities in ancient volcanic mountain area, presents unique peak, column, pier, the hole, wall etc odd rocks is basically a modelling step, geomorphic museum.
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.
所以火星的千层榚地貌，很可能是古湖或古海沈积物所形成的沈积岩。
Likewise, the layered beds on Mars may be sedimentary rock formed in ancient lakes and seas.
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.
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.
分析了浙江省第三系玄武岩的分布范围、喷发旋回、地层岩性、古地理环境； 进行了玄武岩台地的地貌特征分类；
The main research area includes:(1) The distribution range, eruption gyrations, strata lithologic character and palaeogeographic environment of tertiary basalt of Zhejiang is analyzed.
分析了浙江省第三系玄武岩的分布范围、喷发旋回、地层岩性、古地理环境； 进行了玄武岩台地的地貌特征分类；
The main research area includes:(1) The distribution range, eruption gyrations, strata lithologic character and palaeogeographic environment of tertiary basalt of Zhejiang is analyzed.
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