发育史 meaning in Chinese
developmental cycles
developmental history
Examples
- The evolution history of northwest tarim as viewed from the features of piqiang fault
从皮羌断裂发育史想到 - The western hubei - eastern sichuan area is located at the junction belt between the eastern sichuan folded belt in the sichuan basin and xianexi folded belt , belong to eastern extended part , which is similar to the eastern - sichuan structure in many aspects . for example , they share a structural unit , resulting in the same sedimentary history and the same generation - reservoir - seal assembly as each other
鄂西渝东区处于四川盆地川东褶皱构造带与湘鄂西褶皱带的接合部位，属川东褶皱带东延组成部分，具有与川东相似的沉积发育史与生储盖组合；相同的构造发育史与构造形式；类似的天然气藏类型与保存条件。 - The analysis results of hydrocarbon generating history , paleotemperature history , the homogenization temperature distribution of fluid inclusions and individual fluid inclusion compounds show that the natural gas charging times in the center gas field is two . the first is at the age of late triassic . at that time , natural gas migrated from the east to the west and from the south to the north
根据鄂尔多斯盆地中部的沉积史、构造发育史、古岩溶形成史、生排烃史等等，按其时空配置关系，归纳气藏的形成可分为四个演化阶段：储集层孕育阶段（ 0 ； c ； ） 、圈闭形成阶段（ c 。 - The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep . under the background of indian plate subducting under asia - europe plate , bachu forebulge was greatly affected by the development of southwest depression and awati depression . almost all of its structure reversed , and as a result of it , both of its south and north boundary migrated . according to its evolution history and its feature , the authors tentatively use both - side migration model to interpret the evolution of compound forebulge . since triassic , almost all the spheres above lithosphere synchronously became flexure . because transpressional stress field became increasingly strong , bachu forebulge continued uplifting and big faults formed . then , bachu uplift , as a whole , slipped upward along those big faults and showed migrating toward thrust zone in plane . in tectonic tranquility , the lithosphere bounded back and in consequence of it , bachu uplift slipped down and showed migration toward craton , at that moment negative inversion structures developed . while the forebulge migrated toward its south and north foredeep , it was very possible that locally extensional stress appeared in the forebulge
在印度板块向欧亚板块俯冲的大背景下，巴楚前缘断隆受西南坳陷和阿瓦提凹陷的影响，新生代时构造体制发生反转，边界向南北迁移。根据其发育过程特征，作者用复合前缘隆起两端迁移模式对复合前缘隆起独特的构造发育史进行了解释：即三叠纪以来岩石圈各圈层同步挠曲变形。随着挤压应力场的增大，巴楚隆起在挠曲基础上不断抬升，形成几条大型断裂带。