• 本文阐述华南元古代晚期活动陆缘特征

    This paper deals with the features of late Middle Proterozoic active continental margin in South China.

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  • 东亚陆缘地区存在一系列陆缘弧。

    There are a series of epicontinental ares in the marginal regions of the East Asia.

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  • 克里克陆缘地块位于塔里木盆地西南

    Ancient land reason massif crick of iron lie in southwest predestination of tarim basin.

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  • 辉绿瓦纳被动陆缘古生代裂解产物

    Diabase-porphyrite was the splitting product of passive margin of Gondwana Continent in Late Jurassic.

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  • 导致右江盆地由陆内裂盆地向被动陆缘裂谷盆地演化

    It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift basin.

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  • 南海北部陆缘中生代晚期曾形成宏伟华夏陆缘山带

    There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.

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  • 音图陆缘拉张解体阶段源自结晶基底裂解陆块

    Baoyintu Group is recognized as an ancient fragment from crystalline basement in stage of continental margin disjoined.

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  • 滨海区的志留系,成为凯地体陆缘增生组成部分

    TheSilurian on the littoral area has been a part of the Xingkai terrain epicontinental aggradation-al belt.

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  • 断裂构造南海北部陆缘新生代构造作用基本特征

    Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic.

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  • 重点探讨了我目东南沿海陆缘重力异常特征及其形成机割。

    The features and their original mechanism of gravity anomaly of the epicontinental arc in the Southeast China are the focal point in discussion.

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  • 深入探讨了南海东北部表层沉积粉分布格局陆缘植被关系

    The relationship between sporopollen assemblage and vegetation of the continental margin has been discussed.

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  • 前者为陆内-环境产物.后者形成陆缘盆地构造环境。

    The former is formed in trench - arc environment ofintracontinental rift, and the latter in marginal basin.

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  • 杨子地块北缘被动陆缘拉张海盆形成了与沉积有关矿源层。

    In contrast, sedimentation related source beds were traceable to some basins caused by tensional events along the northern margin of the Yangtze massif.

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  • 硅质岩形成环境反映了陆缘小洋侏罗世所处构造背景

    The sedimentary environment of the chert reflects the tectonic setting of the small oceanic basin in Late Jurassic.

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  • 阶段构造组合板块俯冲-碰撞有关,形成缝合-陆缘系统

    The early stage tectonic organize related to the plate subduction, collision forms suture belt and precontinental arc system ;

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  • 活动陆缘板块活动相对地区也是水合物发育有利地区。

    The passive continental margin is a comparatively weak region of plate tectonic movement, but it is a favorable region for gas hydrate.

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  • 温室效应促使南极冰盖(首先陆缘部分融化可能崩溃

    The green house effect will cause that Antarctic ice sheet (especially on the ice shelves) to be partly melt away, but can not destroy it.

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  • 它们形成构造环境陆缘碰撞山环境晚期山后环境演化。

    The tectonic environment of forming these units develops the epicontinental-collison orogenic environment to the late-orogenic or post-orogenic environment.

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  • 文中着重讨论勒巴泉—公婆泉陆缘基本特征形成动力学背景

    This paper focus on the basic characteristics of Lebaquan-Gongpoquan epicontinental arc and the dynamic background for its formation in the contiguous area across Gansu, Xinjiang and Inner Mongolia.

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  • 文章利用天然地震PS转换波研究了北部湾陆缘地区的地壳结构特征。

    By the data of PS-waves of the earthquakes, the crustal structure of the margin of the Beibu Gulf is studied in this paper.

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  • 地块华南地块是中生代早期碰撞缝合在一起的,构成了古南海北部陆缘

    The Indochina block and South China block have collided and sutured together in early Mesozoic, and formed the northern mar - gin of proto-South China Sea Basin.

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  • 台西盆地是中国东南海域新生代陆缘扩张形成一系列东向裂—坳陷盆地之一

    The occurrences of the evaporation ducts of the South China Sea and East China Sea are studied based on the New evaporation duct model and the iron tower platform hydrometeorological data from Jan.

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  • 被动陆缘陆坡深水蕴藏大量油气天然气水合物资源受到石油行业关注。

    The oil industry is interested in the deepwater slope area of passive margin because of its contained large scale of oil & gas and gas hydrate resources.

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  • 小独山西钨矿床位塔里木板块东端,北山陆缘活动带古生代柳园-俞裂谷带西段。

    Xiaodushangxi tungsten deposit is located in the eastern end of the tarim plate, Beishan paleozoic continental margin activity with Liuyuan-Yu Well son with the western part of Rift Valley.

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  • 岩石地球化学示踪地层学研究表明,冈斯带石炭纪为伸展背景下冈瓦纳陆缘陷环境。

    Geochemical and stratigraphical studies suggest that the tectonic setting of the Gangdese region is depressional rifting to the northern margin of Gondwanaland.

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  • 南海北部陆缘NW-SE方向流动地幔存在使得伸展活动具有由北向发育的机制。

    The existence of NW-SE direction mantle flow under the continental crust in the north continental margin of South China Sea made the extension activities migrate from north to south.

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  • 马超营一一潘河大断裂,界定了古生代时期华北板块活动大陆边缘陆架陆缘南部边沿

    The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.

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  • 东亚陆缘新生代盆地几何特征具有相似性,呈nne、NEE至EW向断裂为边界的准菱形。

    The Cenozoic basins of different magnitudes in East Asia continental margins are similar and self similar in shape.

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  • 岩岩石类型火山岩陆缘碎屑沉积岩火山岛弧拉斑系列系列火山岩、绿岩等。

    Their original rocks are volcanic rocks, epicontinental clastic sedimentary rocks, and ophiolite of volcanic and island arc tholeiitic series or calcium alkali series.

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  • 岩岩石类型火山岩陆缘碎屑沉积岩火山岛弧拉斑系列系列火山岩、绿岩等。

    Their original rocks are volcanic rocks, epicontinental clastic sedimentary rocks, and ophiolite of volcanic and island arc tholeiitic series or calcium alkali series.

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