裂谷带

山西裂谷带地壳岩石波速的研究

Investigation of wave velocity of crustal rocks in Shanxi rift zone

试论攀西裂谷带铂钯矿的找矿前景

On Prospecting Potential of Pt-Pd Mineral Resources in the Panzhihua-Xichang Rift Zone

在空间上，K2O的含量大体与日本海裂谷带玄武岩相当，而远远高于日本岛弧玄武岩的含量。

At space , the content of potassium oxide ( K_2O ) is as many as that of the basalt of Japan Sea rift belt , but is much higher than that of Japan Island arc .

1996年至2001年山西裂谷带6期GPS复测资料的基本特征为趋势性活动，表现为北段向西运动，南段向东运动，整体呈逆时针的差异活动性质；

The basic characteristics of the six GPS repetition measurement data in Shanxi rift valley zone from 1996 to 2001 present trending activity , showing the characteristic of differentia activity in anticlockwise as a whole , with the north segment moving towards west and the south segment moving towards east .

该地块自中新世以来向SE方向倾斜是南苏丹裂谷带在后裂谷热沉降阶段造成的裂谷肩块体的向内旋转。

The rotation of the Mellit block toward northwest was the outward rotation of the northwestern shoulder of the South Sudan Rift during the rifting phase , and the rotation toward southeast was the inward rotation of the rift shoulder during the post-rift thermal sag episode .

裂谷带火山喷发区地壳厚度12～50km，岩浆来源深度为270～100km，形成温度约1213～1163℃。

The crust thickness of volcanic eruption area in the rift zone is 12-50 km , the depth of the magma origin is 270-100 km , and the formation temperature is about 1213-1163 ℃ .

大陆边缘裂谷带是矿床形成的大地构造环境。

It is located in the rift of continental margin .

攀西裂谷带中白马杂岩及其单矿物的稀土元素地球化学特征

REE geochemistry of Baima complex in the Panxi rift belt

其大地构造环境为大陆裂谷带。

The tectonic environment suggests a continental rift zone .

论福建省闽中裂谷带成矿系统

On the metallogenic system of central Fujian rift

攀西裂谷带及其邻区的现代构造应力场特征

Characteristics of the recent tectonic stress field of Panxi rift valley zone and its vicinity

区域地球化学不均一性起因初探&以吕梁中条古元古代裂谷带为例

A Preliminary Discussion about Origin of Geochemical Heterogeneity & An Example from Luliang-Zhongtiao Paleoproterozoic Rift

一条正在发育的中、新生代裂谷带

A Mesozoic - Cenozoic rifting zone

忻州盆地和贝加尔裂谷带医疗矿水水化学相似性研究

A comparative study of hydrochemistry on geothermal mineral waters in Xinzhou basin and Baikal rift zone

山西裂谷带形变应力场及其与地震的关系

Analysis of Deformation Stress Field of Shanxi Rift Valley Zone and the Relation between It and Earthquakes

贝加尔裂谷带通京盆地新生代火山岩石学与地球化学特征及其构造意义

Petrological and geochemical characteristics and tectonic implication of Cenozoic basalts in TUNKA basin in Baikal rift belt

从海西晚期至燕山期，在裂谷带广泛发育了不同时代、不同类型的花岗岩。

Different types of granites emplaced at different stages were widely formed from Hercynian movement to Yanshan movement .

走进埃塞裂谷带

Rift Valleys in Ethiopia

在空间上有成带分布特点，主要分布在裂谷带和被动大陆边缘，与同生断裂密切相关。

These ore deposits displaying belteddistribution mainly occurred in rift and passive continental margins , related to the syndepositional fractures .

贝加尔裂谷带是全球典型的大陆裂谷带之一，新构造运动强烈。

With intense neotectonic movement , Baikal rift zone is one of the typical continental rift zones in the world .

（12±2）×10~6a的年龄值是攀西裂谷带内，甚至整个扬子准地台内最年轻的花岗岩年龄值。

12 ± 2 Ma is the youngest age for granitoids in the Panxi rift zone and even in the whole Yangtze Paraplatform .

对我国北方上古生代地层的一些认识博格达造山带是上古生代裂谷带，于石炭纪末闭合。

The Bogda region is interpreted to be an upper Palaeozoic continental rift , which was closed towards the end of the Carboniferous period .

我国东部第二沉降带是从晚中生代开始形成的大陆裂谷带。

" The second subsidence zone " in eastern China is a continental rift systemin the Eastern Eurasia Plate from the beginning of late Mesozoic .

雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；

The Yarlung Zangbo and Bangong-Nujiang belts were twins in the Tethyan ocean , which began to develop into two ocean rift belts in the triassic .

这类矿床多分布在地台稳定区的边缘，常沿深断裂或裂谷带延展方向呈群分布。

They are commonly distributed along the margins of such stable areas as the platform and are characterized by oriented distribution along extensions of deep faults or rifts .

裂谷带内晚古生代火山岩建造发育，深入研究火山岩及其岩石地球化学特征，对分析判别裂谷成因及其演化有重要意义。

Volcanism is developed in Late Palaeozoic . there are important to study on volcanic rocks and its lithogeochemical characteristics of volcanic rocks for the causes and rift evolution .

木洛稀土矿床是攀西地区新发现的中型稀土矿床，位于攀西裂谷带北段西界，冕西稀土成矿带西部亚带。

It is located in north part and west flank of the Panxi rift and belongs to the western sub-belt of REE mineralization in the west of Mianning region .

阿加隆洼亚火金（铜）矿带位于甘孜理塘裂谷带中段，是重要的金矿富集区。

The Ajialongwa-Yahuo Au - ( Cu ) ore zone as an important Au accumulation region lies in the middle sector of the Garz ê - Litang rift zone .

小独山西钨矿床位于塔里木板块的东端，北山陆缘活动带古生代柳园-俞井子裂谷带西段。

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 .

三叠纪及其以前，柴达木地块主体呈现稳定的隆升状态，仅其南、北缘发育的裂谷带时张时合，沉积了一套海相裂谷型建造。

Before and in Triassic period , the main part of Qaidam Massif rose stably , but rift zones developed and received marine rift typed sediments only at southern and northern borderland .