tectonic maps meaning in Chinese
构造图
Examples
- Tectonic map of china , 1 : 4 , 000 , 000 , based on diwa ( geodepression ) theory . map press . beijing . won national scientific congress ' s prize , 1980 ; 2nd ed . , 1980 ; exhibited on 26th igc , paris , 1980
400万中国大地构造图(按地洼学说编制) .地图出版社(与其他单位合编) . (获1978年全国科学大会奖， 1980年再版，被选送巴黎第27届国际地会展出) - The investigation in the field was combined with research indoors . by classifying tectonic sequence , confirming corresponding prototype basin , analyzing paleo - tectonic stress fields in different periods , plotting correlative tectonic map based on 297 explore wells , and analyzing the traits of the remaining depressions producing hydrocarbon and their migration rules in the ordovician , the author studied the basement of the basin ; the fault system of the basin ; the tectonic - sedimentary evolution of the basin and its circumference areas ; the prototype basin and corresponding dynamics background ; the paleo - tectonic patte rn and its evolution in the layers of producing gas in different periods of ordovician ; the superposition relationship among the different period basins formed by different stress fields ; the reformation of the basin and the formation , redistribution and final emplacement of the gas pools
采用野外地质调查与室内综合研究相结合，通过构造层序的划分及其相应盆地原型的确定、不同期次古构造应力场的分析、以297口探井数据为基础的相关构造图件的编制、奥陶系残余生烃坳陷及其迁移规律研究等的综合分析，开展了盆地基底以及盆地断裂系统、盆地及邻区构造与沉积演化、盆地原型及其形成的动力学背景、奥陶系产气层不同时期的古构造格局及其演化、不同期次构造应力场形成的不同世代盆地之间的叠置关系以及盆地改造与天然气藏的形成、重新分配和最终就位诸方面的研究。 - The management work data of oil - field earthquake exploration and oil - well position , which has not only data of current space position , but also entitative attribute data describing , have great capacity , traditional cad graphics describing the data plus the model database managing mode ca n ' t already adapt the modem exploration with well geography information for management work demand , so it is necessary to realize the unique management of exploration and oil - field well space data and attribute data use advanced geography information system ( gis ) technique , this thesis is based on the excellence ' s table ' s top geography information system - the maplnfo software , using the second process technique , the digital relief map and tectonic map as the base map , the earthquake exploration database as the original data , established the gis of the exploration and oil - field well in the area of the liaohe oil - field , realize visualization management , it provides a reference thereunder for the earthquake exploration deplo ying the workload and proceeding the technique design , and completed lots of practical work
油田地震勘探与油井井位管理工作数据量大，既有空间位置数据，又具有实体的属性描述数据，传统的cad制图+属性数据库管理模式已经不能适应现代勘探和井位管理工作的需要，采用先进的地理信息系统( gis )技术，实现勘探和油田井位空间数据和属性数据的统一管理是必然的趋势。本文以优秀的桌面地理信息系统mapinfo软件为开发平台，在此基础上进行二次开发，以数字化地形图、构造图为载体，以地震勘探数据库为数据源，建立了辽河油田范围内的地震勘探和油田管理信息系统，实现了数据的可视化管理，为地震勘探部署工作量、进行技术设计，提供了图形和数据的参考依据。并完成了很多实际工作。 - 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。