the Devonian

The lower structure layer consists of the Sinian to the Devonian, in which the A-Man low ridge is observed.

Deposition of the Devonian and Carboniferous was strongly affected by extensional tectonism.

lower tracheophytes in existence since the Devonian.

The sequence of the strata may be correlated with the Devonian period Bulakebashi Formation in west section of East Kunlun.

The Devonian and Carboniferous strata of Novaya Zemlya can be generally divided into the Barents and Kara facies zones.

In the Ordovician, Silurian Period, the Devonian, Carboniferous, the advent of low amphibians and ancient ancient reptiles.

Laminated siliceous rocks in country rocks might represent the nature of the Devonian hydrothermal sedimentary rocks.

Near the end of the Devonian period, 370m years ago, many species of fish and 70% of marine invertebrates perished. The reason is unclear.

The end of the Devonian was a crucial time for vertebrates.

During the Devonian period, northward of Longmen Mountain structural belt is located in northwest border of Up Yangtzee Ancient Land.

second earliest fossil amphibian ever found; of the Devonian; found in Greenland.

During the Devonian, 410 million years ago, two major animal groups dominated the land.

Near the end of the Devonian period 370m years ago, many species of fish and 70 % of marine invertebrates perished.

It is a new species of placoderm, the type of armour-plated fish that dominated the Devonian oceans for 70m years.

The third period of the Paleozoic era, the Silurian follows the Ordovician period and precedes the Devonian.

Determination of the Au background value and Au geochemistry in the Devonian of the West Qinling and their geological significance

A Study of Depositional System of the Devonian System in South Guizhou-Central Guangxi

The Devonian bioherms in Sanchakou, northwestern Xizang and their implications

Distribution of the Devonian shale in China