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 本文采用地質(zhì)和地球物理相結(jié)合的研究思路,運用多種技術(shù)手段和方法;在充分利用已有構(gòu)造圖資料和構(gòu)造要素資料的基礎(chǔ)上,運用地層層序邊界不整合分析法、地層厚度對比分析法,結(jié)合地震資料的精細(xì)解釋、古構(gòu)造和古地貌的恢復(fù)、構(gòu)造演化史研究、含油氣系統(tǒng)的研究,和區(qū)域和局部、平面和剖面、時間和空間的結(jié)合研究,對塔里木盆地和田古隆起構(gòu)造演化及油氣關(guān)系進(jìn)行了綜合分析,認(rèn)為: ( 1 )和田古隆起為一沉積?剝蝕性古隆起;形成于志留-泥盆紀(jì);其構(gòu)造演化可分為三個階段,即加里東期的抬升剝蝕階段、海西期的沉積階段和喜山期的破壞階段,最終由古隆起演變?yōu)橐恍逼聨А?