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tectonic相关的网络例句

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The high-grade metamorphic terrain of Hengshan located at the hinderland of North China Carton in northern part of Shanxi province, China, is a middle-lower crustal transition area of the typical continental crustal profiles of the Wutaishan—Hengshan—Datong—Jining of the early Precambrian etamorphic terrain in China.The Hengshan gneisses of the amphibolite—granulite facieses metamorphic terrain consist of the TTG gneisses and the horizontal adding mantle materials. The Supracrustal rocks in this area are composed of the mafic volcanic rocks and sedimentary rocks. The plenty of granitoid magma activities are the result of anatexes.

中文题名恒山中深变质岩区构造样式副题名外文题名 Tectonic styles of the high-grade metamorphic terrain of Hengshan 论文作者苗培森导师宋鸿林教授学科专业构造地质学研究领域\研究方向学位级别博士学位授予单位中国地质大学学位授予日期2001 论文页码总数88页关键词中深变质岩区构造地质恒山区域构造地质馆藏号BSLW /2003 /P548 /4 位于华北克拉通近中部的恒山中深变质岩区,亦即恒山高级变质岩区,是从五台山—恒山—大同—内蒙集宁这一浅变质岩区至中深变质岩区的我国早前寒武纪典型大陆地壳剖面代表中下地壳过渡带的地区。

In northeastern of basin, together with the structural framework of slope belt and the dynamical information of well, we can conclude that the gas reservoir in Taiyuan-early Shihezi formation dominantly belong to protogene depositional gas reservoir under the normal pressure, and the gas favourable reservoir belt was controled by framwork of main sandbody; But in upper Shihezi Formation to Shiqianfeng Formation the gas reservoir show the feature of secondary Tectonic-depositional gas reservoir under the extremely low pressure, and the gas favourable reservoir belt mainly locate in a zone which the low amplitude structure and main sandbody superposed in the slope belt.

5盆地东北部斜坡带构造与钻井生产动态资料的相关分析结果表明,太原组-下石盒子组气藏主体属于正常压力下的原生岩性气藏,其有利含气区带主要受控于主砂体分布格局;上石盒子组-石千峰组气藏则主要为异常低压下的次生构造-岩性气藏,其有利含气区带主要分布在斜坡带低幅度构造与主砂体叠合区。

It has the metamorphic rock sight—"the Inartificial Gallery" which is black and white, devious and whirlabout and likes the reversal cloud-mist and rising sun, the granite vein injecting along the bedding of gneiss crossing the river-gorge—"the White Dragon Crossing River", nine veins apposing on the rock wall—"the Nine-dragon Wall","the Inartificial Wall " formed by the paragenesis of the level joint and the vertical joint, and the small and exquisite undercutting cave which is the wonder of the new tectonic movement.

有黑白相间、曲折盘旋,如云雾翻卷,似霞蔚蒸腾的变质岩景观――&天然画廊&,有沿片麻岩层理贯入的花岗岩脉,横跨河谷的&白龙过江&,有九条岩脉并列在岩壁之上的&九龙壁&,有水平节理与垂直节理巧妙共生而形成的&天然城墙&,有新构造运动遗迹――小巧玲珑的淘蚀洞穴。

Taiwan lies where the Eurasian and Philippine sea tectonic plates meet and is geologically frail. Notably, the 921 earthquake broke up the rock stratum in many areas and has increased the danger of avalanching and debris flow.

台湾地区位处欧亚板块和菲律宾海板块之交接处,地质脆弱,然而九二一地震后,使得原本破碎的岩层易发生崩塌之行为,致使土石流发生之机率比地震前大许多。

They concluded that clashing tectonic forces were growing in Beichuan, ready to burst in an explosion of seismic energy.

科学家的结论是,地壳撞击的能量在北川聚积,并将以地震的形式释放出来。

They concluded that clashing tectonic forces were growing in Beichuan, ready to burst in an explosion of seismic energy.

他们的结论是,挤压中的地层力量正在北川增长,准备好了在地震能量的爆发中突现。

This research achievements is the result at the base of field geologic data colligating with the data of some drilling and seismic, and of the combining of sedimentology and tectonic geology researches, theory and practice researches, actual measurement of skeleton sections and observation of complemented sections, macroscopical studies and microcosmic studies. The classification and characteristics of sedimentary system and the genetic types and expression form are systematically analyzed in the thesis, and the division scheme of the Youjiang basin is put forward.

研究成果是以大量的野外地质资料为基础,综合了部分钻井和少量地震等资料,采取沉积研究和构造研究相结合、理论研究和实际研究相结合、实测基干剖面与补充观察剖面研究剖面相结合、宏观研究和微观研究相结合的方法,系统地分析了右江盆地的沉积体系种类和特征、层序界面的成因类型和表现形式,进而提出了右江盆地的层序划分方案。

Also the question of how heat is transported as the lithosphere forms and evolves on scales ranging from tectonic plate, to melt generation and migration into the crust, to transfer of heat from hot rock to convecting fluid, is addressed.

在岩石圈形成和发展过程中(从构造板块到熔岩产生、迁移进入地壳,到热从高温岩石到对流海水),详细论述了热的传输机理。

According to the geomorphological structure and the origin of the Loess Plateau with reference to the average uplifting velocity of the gorge district between Shanxi and Shaanxi, it is demonstrated that the Loess Plateau is a unique type of accumulated plateau differing from the familiar plateau types, such as, denudated plateau, tectonic plateau and lava plateau etc..

根据黄土高原的地貌结构与成因,结合晋陕峡谷区新生代晚期地壳平均抬升速度的讨论,论证了黄土高原在成因类型上完全不同於剥蚀高原、构造高原、熔岩高原等各种高原类型,它是一种独特类型的叠加高原。

In this dissertation, sedimentology, historical geology, structural geology, geophysics, structural dynamics/geometric, plate structure etc were combined properly. Taking Jiyang depression as studying object, fault distribution of different periods was analyzed, and thus discussing their structural dynamics. Using tectonic subsidence history modeling and denudating relationship between hanging wall and foot wall in Mesozoic faults, fault activity characteristics were discussed.

本论文将沉积学、地史学、构造地质学、地球物理、构造几何学和运动学、板块构造等多学科有机的结合,以济阳坳陷为研究对象,采用各时期断裂分期配套,分析了不同构造运动时期济阳坳陷断层展布,进行构造运动学讨论;利用构造沉降史模拟与中生代断层上下盘剥蚀关系的恢复,探讨了中生代断裂活动的特征。

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