tectonic sequence meaning in Chinese
构造序列
Examples
- Classification of tectonic sequence and dynamic evolution of jixi basin , eastern heilongjiang province
黑龙江东部鸡西盆地构造层序划分与盆地动力学演化 - Through studying the stratigraphic framework of tectonic sequence , the characteristics of deposits and multi - episode tectonic movements show the eastern qinling and dabie orogenic movement and basin formation processes
晚白垩世至古近纪区域构造背景发生重大变化，构造层序记录了晚燕山期地壳快速均衡隆升，伸展断陷盆地形成演化过程。 - Through comparing the tectonic sequences stratum of triassic - paleogene period in the east of hubei , in jingmen - dangyang basin , in zigui basin and in the northeast of sichuan , on the southern margin of the eastern qinling and dabie orogenic belt , three main tectonic sequences are divided
摘要通过对东秦岭大别山造山带南缘鄂东地区、荆当盆地、秭归盆地和川东北地区三叠纪古近纪的构造层序对比研究，划分出三个大的构造层序，并分析了中上扬子地区印支期以来沉积盆地性质转换和迁移过程与构造层序的耦合关系，揭示了东秦岭大别造山与成盆作用过程。 - 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 basin has three evolutionary stages including intracontinental rift basin in p1 - p2 , down basin in t2 + 3 - k and the strong trust - orogeny process in n - q . according to the unconformity contact relationship and sedimentary components , santanghu basin is divided into four tectonic sequence such as : o - c tectonic sequence of basement , pi - p3 tectonic sequence , t - k tectonic sequence and n - q tectonic sequence
根据盆地地层之间的不整合接触关系，考虑到各层序沉积物组成与生物组合特征等因素，将三塘湖盆地划分为： ( o ? c )基底构造层序，二叠系( p )构造层序，三叠系( t ) ?白垩系( k )构造层序和第三系、第四系构造层序。