inversion structure meaning in Chinese
倒转构造
Examples
- Sichuan basin ; extension compression ; dynamical environment ; extensional structures ; inversion structures
四川盆地拉张-挤压动力学环境伸展构造反转构造 - Structural characteristics of inversion structure , fold association style , thrust fault zone upright strata developed belt shown in great profiles were also discussed
对剖面中反映的构造反转、褶皱组合样式、逆冲断裂带、直立地层发育带的构造特征进行了探讨。 - Viewing from the global tectonics , the authors dynamically described the dialectical relationships between extensions and compressions in time special 4 - d , and pointed out the different tectonic deformation systems corresponding to different tectonic dynamical environments . considering the geological evolution of sichuan basin , from nine aspects , the authors proved that the tectonic dynamical environments of sichuan basin , after its formation , has experienced the early extension , middle transition and late compression environments . correspondingly , as the paper suggests , a considerable attention need to be paid to the comprehensive studies of the early extensional structures , middle inversion structures and the late compression structures of sichuan basin when analyzing its tectonics
从全球构造着眼，动态地从时间-空间四维阐述了拉张-挤压构造动力学环境的辩证关系，指出了不同构造动力学环境对应于不同的构造变形系统。结合四川盆地地质演化历程，从9个方面论证了四川盆地自其形成以来，构造动力学环境曾经历了早期拉张中期过渡晚期挤压的过程，相应地在对四川盆地进行构造分析时，要注意早期伸展构造中期反转构造晚期挤压构造的识别和综合研究。 - 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。