裂陷槽 meaning in Chinese
taphrogenic trough
Examples
- Yanqi basin , located in the northern wing of the " v - type " thrust - fold belt , is related to the reversion of the kuluketage aulacogen
因此库鲁克塔格裂陷槽的构造反转是焉耆盆地构造变形的主要力学来源。 2 、描述了盆地内的构造样式。 - 4 . the accurate position where the carbonate reservoir existed in feixianguan group in taphrogenic trough has been figured out , which usually located in the half cycle when the base level falls
4 、明确了川东北地区裂陷槽中飞仙关组储集层在层序地层中发育的位置。 - Cihai iron ore deposit is a subvolcanic - ore pulp intrusive - hydrothermal scouring replacement deposit , which is occurred in the rift of the southern margin of the eastern tianshan mountains in the lower permian epoch
摘要磁海铁矿床产于早二叠世东天山南缘裂陷槽大地构造环境中，为次火山矿浆侵入热液充填交代矿床。 - Beginning form relation of basin - mountain , the tectonic evolution and the petroleum system and pool - forming process have been studied with the integration of structural physics modeling , balance profile reversion and other new testing technology . the main innovative achievements of the dissertation can be summarized as following : 1 . on the basis of comprehensive analysis of yanqi basin relationship to tianshan orogenic belts , it was suggested that kuluketage faulted - upheaval was an aulacogen in early paleozoic , which undergone multiple opening - closing along with tianshan orogenic belts , and suffered extensively compressing in late hercyhian cycle and formed a " v - type " thrust - fold belt
论文总的指导思想是以现代石油地质理论为基础，以整体、动态、系统、综合分析为原则，以成盆?成烃?成藏研究为主线，运用正、反演相结合的残留盆地油气成藏系统评价思路，采用构造物理模拟、平衡剖面复原和多种测试新技术，从盆山耦合关系切入，研究含油气系统成藏要素及其相互作用过程，探讨油气成藏主控因素和油气分布的有序性，取得如下创新性成果和认识： 1 、系统分析了焉耆盆地形成演化与天山构造带的关系，提出盆地南侧的库鲁克塔断隆在早古生代为一大型裂陷槽，之后随着天山构造带的演化，经历了多次开合运动。 - 2 . the new idea about classification of oil and gas accumulation unit for exploration have been put forward , which holds the sound basis for the perpendicular and plane position and prediction of carbonate reservoir in feixianguan guan group . 3 . the depositional systems of feixianguanguan group in taphrogenic consist of carbonate platform facies ( include oolitic bar , oolitic beach , lagoon , flats ) , margin shelf and trough . there are five development staged in taphrogenic trough
3 、指出裂陷槽中飞仙关组沉积体系在平面上由碳酸盐岩台地相(包括滩坝相、鲕滩相、泻湖相、潮坪相) 、陆棚相、裂陷槽相组成，裂陷槽经历了发生期、发展期、稳定期、过渡期及衰亡期五大发展演化阶段，每一阶段各发育不同的沉积相，且以一种沉积相为主。