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加里东

网络Caledonian

加里东

加里东

加里东

Caledonian

欧美习用,加里东 (Caledonian)构造阶段(Z-Pz1),海西 (Hercynian/Variscan)（华力西）阶段（ Pz2），老阿尔卑斯阶段(Old Alpe…

1

These high precision dating date provide constrains on the timing and nature of the Caledonian Movement in the Wuyi Mountains.

这些新的高精度年龄学数据为武夷山加里东构造运动时限和性质提供了精确约束。

2

From the Early Silurian large scale of retrogression had begun accompanying the Late Caledonian movement .

晚加里东运动（始于早志留世）发生了大规模的海退。

3

Widespread magmatic rocks , the area from the east to the Himalayan period since the intensity of the magma activity times .

区域普遍分布的岩浆岩，是从加里东期至喜马拉雅期以来分歧强度的多期次岩浆勾当的产物。

4

They also do not belong to the south meta-volcanic rock series of Northern Qilian Caledonides tectonic belts .

也不属于北祁连加里东构造带南带变质火山岩系的一部分。

5

In Europa are similar suitable locations for ELF transmitters , to be found in areas covered by the Baltic and the Caledonian shields .

在欧洲，合适建造 ELF 发射机的位置在波罗的海地盾和加里东地盾覆盖的区域。

6

The Early Caledonian movement resulted in a pseudo-conformity between Cambrian and Lower Ordovician .

早加里东运动，造成下早奥陶统与寒武系的假整合；

7

The paper focus on the horizontal and vertical characters of tensional normal fault formed in the early Caledonian .

着重分析了加里东早期张性正断裂的平面和剖面特征。

9

the South Qinling orogenic belt is the combined mountain chain resulted from late Caledonian and Hercynian-Indosinian movement .

南秦岭造山带是晚加里东和海西 -印支运动形成的复合山链。

10

Results There are the key metallogenetic events during the Caledonian, Indosinan and Yanshanian periods in the Qinling Orogeny .

结果秦岭造山带存在加里东期、印支期和燕山期的几个关键成矿地质事件。

11

The three times of oil generation of middle - lower Ordovician source rocks happened in late Caledonian , Yanshanian and late Hercynian.

中下奥陶统烃源岩主生油期有三个，分别为：加里东中晚期、燕山期、海西晚期。

12

While the later activity of shear fault in Caledonian event should have triggered the landsliding .

而加里东期走滑断裂的后期活动成为山体滑坡的触发因素。

13

Post Caledonides platform also did not exist , there was an ocean basin and could be a part of the Paleo Tethys;

华南不存在加里东后地台，而存在晚古生代洋盆，它可能是东特提斯洋的一部分；

14

Rock Hill Caledonian granite and marble ago 4 - 6 billion years.

山体岩石为加里东期花岗岩和大理石，距今 4——6 亿年。

15

Determination of the age of gold deposits in southeastern Guizhou: with a discussion of the Caledonian Hunan -Guizhou gold ore belt

黔东南金矿形成时代的确定兼论湘黔加里东金矿带

16

Characteristics of Caledonian Karstification Reservoir in Tahe Oilfield and Its Distribution

塔河油田加里东期岩溶储层特征及分布预测

17

New information of Caledonian tectonic features in the northern part of the southeastern margin of the Lower Yangtze valley

下扬子东南缘北段加里东期构造形迹新资料

18

Caledonian Convergent Transformation and Metallogenetic Response in the North Qilian Mountains

北祁连山加里东期聚敛作用的构造转换及其成矿响应

19

Caledonian tectono -thermal event in Tongbai -Dabie orogenic belt and its significance

桐柏 -大别造山带加里东期构造 -热事件及其意义

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