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向北

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In the environment of pressure stress field that caused by the movement toward north of India, Australia and Pacific plates to the south and east, a strong intracontinental subduction overprinted on the deep delamination. of Dabie orogenic belt, and the subducting sediments of Yangtse plate were melted to form the "syncollision" peraluminous granite of this epoch.

在中国大陆南部和东部的印度、澳大利亚和太平洋板块的北向运动所造成的NS向挤压应力场环境中,大别造山带在深部拆沉作用的基础上,又叠加了一次强烈的陆内俯冲作用,俯冲的扬子板块沉积物质熔融形成该期"同碰撞"过铝质花岗岩。

It begins off the east coast of Taiwan and flows northeastward past Japan, where it merges with the easterly drift of the North Pacific Current.

自菲律宾开始,穿过台湾东部海域,沿著日本往东北向流,在与亲潮相遇后汇入东向的北太平洋洋流。

The south and north of the windward side of the Annam Cordillera show great difference in the diurnal variation of rainfall, which is related to migration of rainfall. Rainfall over coastal areas of the Thailand Gulf in 01-04LST migrates to inland northeastwards and then heavy rainfall occurs over areas southwest of the Annam Cordillera in 16-19LST, after that heavy rainfall migrates northwestward along the Annam Cordillera to areas northwest of the Annam Cordillera in 01-04LST in the next day. The migration of rainfall results in different characteristics of diurnal variation on the windward side of Annam Cordillera.

长山山脉西侧迎风坡的一南一北两个区域,表现出明显不同的降水日变化特征,其原因与降水的传播有关。01-04LST,降水大值区出现在泰国湾东部沿海,并向中南半岛岛内传播,16-19LST在长山山脉西南侧形成降水大值区,之后降水进一步沿山脉向西北传播,并于次日01-04LST传到长山山脉西北侧区域,通过降水的这种传播特征从而导致长山山脉迎风坡一侧不同的降水日变化特征。

The stress fields from middle and large scales of mantle convection may jointly lead to the northwestward rifling of Japan, the southeastward rifling of Sea South China Sea, and specific tectonic features of the Ryukyu and Philippine arcs.

中尺度和大尺度地幔流应力场的共同作用,可以解释日本海盆北西向和南海海盆东南向的不对称扩张特性,及各段沟弧系的构造活动差异。

The predicted sand bodies are distributed in north-cast and approximately north-south orientation. The sandstone reservoir, which is getting thin and pinch out to the high west-north structure, is easy to form the lithological trap with sand body updip pitchout and the structural lithologic trap. Lens sandstones developed and are distributed in source rocks, It is easy to form lithologic traps.

预测砂体分布呈现出北东向、近南北向展布特征;向西北构造高部位方向变薄尖灭的储集砂体极易形成上倾尖灭岩性圈闭及构造-岩性圈闭,透镜体砂岩也较发育,其分布于生油岩区,容易形成岩性圈闭。

By means of different subjects and te chniques,the paper makes an overall study on the crustal stability of Beihuaiyang region and its adjace nt areas from the aspects of current t ectonic stress fields,principal fa ult structures,analysis of regional fa ults and neotectonic activity,seis mic activity and numerical modeling,etc.

运用多学科、多技术相结合的研究方法,从现今构造应力场特征、现代地壳形变特征、主干断裂构造以及区域断裂活动性分析、新构造运动、地震活动、数值模拟等方面入手,对北淮阳及其邻接区地壳稳定性进行了全面而系统的研究,指出本区地震活动受走滑活动断裂控制,中、强地震集中于区内东南部和西北部NW向与NE向断裂交汇处;第四纪无大规模差异升降运动;数值模拟等综合分析表明,信阳地区的区域构造稳定性高,现代地壳形变量小,应力平缓,地震活动少且弱。

The coal bearing strata in Huainan area is situated in the south-east portion of the North China platform,a synclinorium with northwest by west.

淮南地区构造位置处于华北地台东南部,是一呈北西西向展布的复式向斜。

There are five second tectonic unites: Pabei thrust belt; kangsu-wulukeqiati synclinorium belt; Jilegeyoute synclinorium belt; Tianshan thrust belt; and Wuqia-Kashi tectonic belt.

喀什凹陷被划分为五个次级构造单元:帕北对冲带,康苏-乌鲁克恰提复向斜带,吉勒格尤特-乌布拉克-哈勒马艾列克复向斜带,天山山前冲断带,乌恰-喀什构造带。

The results show that(1)the barrier and passage effects of longitudinal range-gorge break the law of zonal distribution of air temperature in Yunnan,the law of longitudinal distribution of air temperature is obvious and the spatial distribution is very zonally asymmetry;(2)under the effect .

结果表明:(1)纵向岭谷地形的"阻隔—通道"作用,使云南温度的纬向分布规律被破坏,经向分布规律比较明显,空间分布极不均匀;(2)纵向岭谷作用下云南热量地域分布差异显著,南部热量丰富,北部欠缺,西部比东部丰富,河谷地区热量最丰富,滇西北及山区热量最贫乏;(3)6、7月热量最丰沛,1月最为贫乏,春季热量好于秋季;(4)近30 a云南年平均气温有明显的上升趋势,存在明显的7 a、11 a、18 a周期振荡;(5)云南年平均气温具有大范围位相一致的变化趋势及东部冷与西部暖的变化类型。

Chaijiazhuang gold mine located in Lizhiyuan-Diaobazhi gold ore deposit belt that belong to North Qinling Caledonian folded belt of West Qinling folded system and hosted in Danfeng Group that belong to exocontact of Chaijiazhuang adamellite.

柴家庄金矿位于西秦岭褶皱系北秦岭加里东褶皱带李子园—吊把子金矿带上,赋存于柴家庄二长花岗岩体外接触带的丹凤群地层中,严格受NE向及NNW向断裂控制。

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