1.Ocular complications of Rift Valley fever outbreak in Saudi Arabia
沙特阿拉伯暴发的Rift山谷热的眼部并发症
2.In the period, I had taken part in the Europen Union Corinth Rift Laboratory 3F (Faults, Fractures & Fluids) -Corinth Porject and Germany Potsdam Kaiser Bahnhof building strain detecting project.
在此期间参与了欧盟的Corinth Rift Laboratory中的3F(Faults,Fractures & Fluids)-Corinth研究项目和德国的Potsdam Kaiser Bahnhof建筑现场应变监测项目,这些项目的特点是光纤Bragg光栅传感器的应用的工程化。
3.Interestedly, sixteen of the high-crossability accessions were collected from the same place, southeast of the Great Rift Valley in Ethiopia.
令人感兴趣的是,这20个高亲和性的品种有16个都处于埃塞俄比亚的Great rift valley的东南方向。
4.SEQUENCE STRATIGRAPHIC MODELS FOR A RIFT LACUSTRINE BASIN-AN EXAMPLE FROM THE JIYANG DEPRESSION IN THE BOHAI BAY BASIN
SEQUENCE STRATIGRAPHIC MODELS FOR A RIFT LACUSTRINE BASIN－AN EXAMPLE FROM THE JIYANG DEPRESSION IN THE BOHAI BAY BASIN
5.Based on the data of gravity-magnetic anomaly,tectonics and strata from rift terrain in Eogene in the shelf basin,East China Sea,this paper demonstrates the genetic factors for strata developed in rift periods, and discusses the controlling influence of basement for rift boundaries,structure pattern and deep-cutted strike-slip faults and rift geographical features controlled by faults.
以东海陆架盆地早第三纪裂谷区内若干盆地的重磁、构造、地层资料为基础,讨论了裂谷期成因地层控制因素. 重新认识了基底对裂谷边界、构造格局、深切平移断裂的控制作用以及受断裂控制的裂谷地貌特征.
6.Minxinan-Yuedong rift valley system, Dian-Qian-Gui rift val-ley system, and the rift ditch-rift valley system of middle-late devonian period in south China and so on.
这种构造主要有峨眉山张裂玄武岩高原、湘东裂谷系和湘南古地幔柱、闽西南一粤东海西印支裂谷系、滇黔桂裂各系和中晚泥盆世华南裂沟一裂谷系等。
7.Viewing from the global scope, particularly looking at the situation in China, the granitic tectono-magmatic assemblages could be divided into five major types: (1) oceanic crust subduction type, such as continental margins on both sides of the Pacific Ocean; (2) continent continent collision type, e.g., the Himalaya-Gangdise collisional belt; (3) extensional continental margin type, such as the Southeast China extensional margin and the Basin and Range Province, USA; (4) inland faulted depression type, such as the Lower Yangtze faulted depression and the Qiantan-Xinjiang faulted depression; (5) rift type, such as the Eastern African Rift and the Panxi Rift of China.
从全球范围来看，结合中国的地质实际，花岗岩的构造岩浆组合可以区分为5种主要类型：(1)洋壳俯冲消减型，如太平洋两岸的大陆边缘；(2)陆－陆碰撞型，如喜马拉雅－冈底斯碰撞造山带；(3)陆缘伸展型，如中国东南部伸展型大陆边缘、北美西部盆岭省；(4)陆内断裂拗陷型，如长江中下游断裂拗陷、钱塘江一信江断裂拗陷；(5)裂谷型，如东非裂谷、攀西裂谷。
8.The study of basin geometry,filling paterns and sequences and regional tectonic framework of the Eogene basins reveals that the Yishu Graben,recognized as an incipient rift basin,is ascribed to a part of the Cenozoic rift systems in northeastern China. which is developed poorer than the Liaohe rift basin system,but better than northern Jiayi Graben.
伊舒地堑早第三纪盆地的结构、充填形式和充填序列以及区域构造格局表明,它属于我国东北部(东部)新生代裂谷系中的一部分,其发育级别低于辽河裂谷盆地带,而优于佳伊地堑北段,为一初始裂谷盆地。
9.Since Lower Devonian to Middle Permian Maokou period, the Hercynian movements which relied on extension motion began in the south China plate and Sanjiang tectonic area in the west of south China Plate, the deposition and the tectonic evolution of south China had characters of passive continental margin, which was characterized by intracontinental rift basin to passive continental margin rift basin for the basin type.
自早泥盆世至中二叠世茅口期,华南板块和西边的三江构造区开始了以伸展作用为主的海西运动,中国南方的沉积、构造演化具有被动大陆边缘的性质,盆地类型则从陆内裂陷盆地演变为被动陆缘裂陷盆地。
10.(6) Like Red Sea, the velocity (0.20～0.28cm/a) and distance (240～336km) of the rift tectonic opening were small. However, the velocity (3.5～5.0cm/a) of rift closing was large, like the Andes type.
（6）本区裂谷拉张速度（0．20～0．28cm／a）、距离（240～336km）小（近似红海），而闭合速度（3．5～5cm／a）大（近似安第斯）；
