Using seismic , logging , and assaying data , and combined with vitrinite reflectance erosion thickness restoration method and seismic stratigraphy paleogeomorphology restoration way , we have restored caledonian paleogeomorphology in the central area of tarim 摘要利用地震、测井和分析测试资料，结合镜质体反射率剥蚀厚度恢复法和地震地层学古地貌恢复法，对塔中地区中加里东期古地貌进行了恢复。
Paleogeomorphology framework is controlled by regional tectonic movement change , and it has impact on sedimentary ratio change , sedimentary center transference , and sediment preservation , at the same time , paleogeomorphology framework restricts the types of facies and plane distribution of facies zone 古地貌格局的变化受控于区域构造运动变化，影响着沉积速率变化、沉积中心迁移及沉积物保存，制约着塔中地区的沉积相类型及沉积相带的平面展布。
Then this paper discusses the main control factors of lithological traps . the types , features and the distributional area of theses depositional systems are dominated by macro paleo - geomorphic units . and the exact position of these lithological traps are determined by local paleo - geomorphic units 古宏观地貌(凸起、洼陷与大型沟槽)控制了沉积体系的类型、沉积特征及至储集体的分布范围；局部古地貌(断槽、地堑、断阶、沟谷等)决定了岩性圈闭发育具体位置。
The structural slope - break zones are defined as the depositional slopes abrupt change in geomorphology and developed widely in fault and foreland basins , the recognition of which is significant for predicting the distribution of depositional systems tracts , particularly the lowstand systems tracts which usually comprised economically important reservoirs in these basins 构造坡折带是由构造活动所产生的、对沉积作用具有长期控制作用的古沉积斜坡或古地貌突变带，在断陷或前陆等盆地中普遍发育，其识别对阐明盆内沉积体系域，特别是构成重要油气藏的低位域的分布和预测具有重要意义。
Karst cycle ii could reconstructed the middle and upper ordorician , and the cave preservation of the karst cycle ik iii are better than the cave of the karst cycle i . 5 ) the genetic forecast mode of karst reservoir in the tahe oilfield are founded on the basis of the research of pleokarst topography , pleodrainage system and karst cycle 岩溶旋回可改造中上奥陶统，岩溶旋回、的洞穴保存情况好于岩溶旋回中的洞穴。 5 )通过岩溶古地貌、古水系和岩溶旋回的探讨，初步建立了塔河油田奥陶系碳酸盐岩岩溶型储层成因预测模式。
By now international exploration for subtle trap is mainly used with paleogeography , which integrates geology , geophysics , geochemistry and drilling , among them , seismic method is getting more and more important . there are a couple of favorable conditions to form subtle trap reservoirs , which are dustpan structure , coexisted slope and sag framework , etc . they lead to form multiple and extensive non - structural traps 目前，国内外勘探隐蔽油气藏的方法主要是岩相古地理和古地貌分析法，常用的手段是地质、地球物理、地球化学和钻井方法的综合，其中地震方法在隐蔽油气藏勘探中起到了越来越重要的作用。
The study area was studed in sequence stratigraphy which was directed by the theory of h . posamentier , and high frequency sequence stratigraphic framework was built base on seismic and drilling analysis , furthermore , cooperating the interpreted result of seism and drill to identity and divide sediment facies can recover paleogeomorphic and paleogeographic environment , and predict profitable oil trap 本文在h . posamentier高分辨层序地层学理论的指导下，分别从钻井、地震等方面对整个上区进行较为详细的层序地层分析，建立起高精度的层序地层格架。并结合地震、测井解释的结果进行沉积相的识别利划分，恢复古地貌和古地理环境，进而对有利区带进行科学的预测。
On the base of fully utilizing the available data about tectonic maps and structural elements , the present paper has made synthesized research that used the ways of stratigraphic sequence edge unconformity analysis and stratigraphic thickness correlation analysis , and combined seismic - data interpretation , review of paleo - structure and ancient landform and research of tectonic evolution and petroleum system , and combined region and location , plane and profile and time and spatial . by the synthesis analysis on tectonic evolution of hetian paleo - uplift in tarim basin , the results indicate that : ( 1 ) hetian paleo - uplift is a sedimental and erosional paleo - uplift . the formation and evolution of the hetian paleo - uplift experienced three stages , that is , the uplifting and eroding stage of the caledonian period , the depositional stage of the hercynian period and the destroying stage of the himalayan period , and evolved from paleo - lift to inclining strap at last 本文采用地质和地球物理相结合的研究思路，运用多种技术手段和方法；在充分利用已有构造图资料和构造要素资料的基础上，运用地层层序边界不整合分析法、地层厚度对比分析法，结合地震资料的精细解释、古构造和古地貌的恢复、构造演化史研究、含油气系统的研究，和区域和局部、平面和剖面、时间和空间的结合研究，对塔里木盆地和田古隆起构造演化及油气关系进行了综合分析，认为： ( 1 )和田古隆起为一沉积?剥蚀性古隆起；形成于志留-泥盆纪；其构造演化可分为三个阶段，即加里东期的抬升剥蚀阶段、海西期的沉积阶段和喜山期的破坏阶段，最终由古隆起演变为一斜坡带。
