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志留世

网络Ludlow-Pridoli

志留世

志留世

志留世

Ludlow-Pridoli

...留世地层展布形态、发育特点、构造古地理特征从晚志留世(Ludlow-Pridoli)开始, 佳-蒙地块进王成文等: 中国东北及邻区晚 …

1

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。

2

In the Early Silurian, the Northern Qilian - Hexi Corridor transforms from back -arc survival basin to foreland basin.

早志留世北祁连 -河西走廊由弧后残馀盆地向前陆盆地转化。

3

The Lujiaogou Conglomerate is the sedimentary response to arc -continental collision during the earliest of Silurian.

鹿角沟砾岩标志著弧 -陆碰撞最早发生于早志留世早期。

4

Lithofacies palaeogeography of the Early Silurian in Sichuan area

四川地区早志留世岩相古地理

5

The Faunas and Its Significance of Southern Tianshan Mountains of Xinjiang in the Middle Silurian

新疆南天山中志留世生物群及其意义

6

During upper Silurian-Devonian , the basin is in extrusion state , and turn up large scale uplift ;

晚志留世 -泥盆纪盆地处于挤压状态，出现了大范围的隆起；

7

The Middle and Late Silurian Marine Volcano Eruption Cycle and Volcano Action Evolution of Gongpoquan Copper Ore Field, Gangsu Province

甘肃公婆泉铜矿田中 ―晚志留世浅海相火山喷发旋回及火山作用演化

8

Discovery of Early Silurian graptolite fossils in the Qimantag Group in the western sector of the East Kunlun

东昆仑西段祁漫塔格群早志留世笔石化石的发现

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