Silurian

The long distance thrust system is composed of Ordovician and Silurian and some part of it shows as a klippe.

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

But as the ecosystem recovered after the freeze, it expanded, with land plants becoming common over the course of the Silurian period.

Maokou Formation is one of the major pay zones of Sichuan Basin, in which there are Yangxin Series and Silurian potential source rock.

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

But it was not until the late Silurian before they resembled modern plants.

The strata and lithological traps of Devonian and Silurian are the exploration targets in LS area, Tarim Basin.

Silurian-Devonian island-arc volcanic formation may be hosted in rock full of porphyry copper deposits.

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

The discovery of the Silurian- Devonian oil and gas reservoir reveals a good exploration prospect.

Microscopically, there are two types of occurrence for the bitumen in the Silurian sandstones: one is massive, and another is disseminating.

The contact relationship between Silurian and Devonian is parallel unconformity .

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

Steeply dipping Middle Ordovician Austin Glen Formation (on right) overlain by moderately dipping Upper Silurian Roundout Formation.

Porphyry mineralization, occurred in the Silurian Period, finally formed ore bodies.

Lichuan synclinorium from Silurian System to Triassic System has 7 combinations of oil source rock, reservoir and cap rock .

The asphalt, movable oil and gas shows are quite abundant in the Silurian reservoir in the Tazhong uplift.

In addition, in the late Ordovician, Carboniferous and Silurian, tazhong area may have small-scale volcanic activity.

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

Application of Quantitative Grain Fluorescence Technique in Study of Silurian Palaeo-Oil Pools Distribution in the Center Tarim Basin

Stratigraphy, sedimentary characteristics and lithofacies palaeogeography of the Silurian in Tarim Basin

Recognition of the classification, biostratigraphy and biogeography of the Ordovician and Silurian rugose corals in the Yangtze Region

Accommodation change and its relationship to hydrocarbon accumulation in the Silurian, Tarim Basin

Lithofacies palaeogeography of the Early Silurian in Sichuan area

Sedimentary facies changes in the Silurian Ningqiang Formation in the northern part of the Longmen Mountains

Sequence stratigraphic subdivision and sedimentary system characteristics of Silurian in Tarim Basin

Characteristics of the Lower Sandstone Member reservoir of Lower Silurian in eastern Tarim Basin

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

Non-traditional method for evaluating physical property of Silurian bitumen sandstone reservoirs in Tarim Basin

On the rock hierarchical units characteristics and the emplacement mechanism of Silurian granite in the boundary between Hunan and Jiangxi

Ordovician- Silurian sedimentation and diagenesis in northeastern Tarim basin

The Silurian-Devonian boundary in Baizitian, Yanbian, Sichuan and its geological implications

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

Experimental identification of the structure safety in the section of Silurian slate with sandwiched phyllite in Wushaoling Tunnel

Controlling Factors of Silurian High-quality Reservoirs in Tarim Basin and Selection of Exploration Direction

Stratigraphic Division, Correlation and Geologic Significance of Silurian in Tarim Basin

Silurian High Resolution Graptolite Biostratigraphy and Biotic Recovery in Ziyang, China

The Element Geochemical Features of Ancient Oceanic Sedimentary Environments in the Silurian Period in the Tarim Basin

Characteristics and controlling factors of Silurian reservoir in northern slope of central uplift in Tarim Basin

Silurian-Devonian Intrusive Rocks and Tectonic Environment in Copulae of Kunlun-Qinling Mountains

Determination Methods of Effective Thickness of Silurian Bituminous Sandstone in the Tarim Basin

Geological features of Silurian lead-zinc deposits in the Xunyang area, Shaanxi, China, and direction for ore finding

Petrology and geochemistry of siliceous rocks in Silurian lead-zinc deposits of southern Qinling region

Properties and Controlling Factors of Lower Silurian Reservoir in Kalpin Area, Tarim Basin

Geological characteristics and distribution of oil and water in Silurian buried hill reservoir in Yaerxia oilfield, Jiuxi basin

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

Sedimentary Characteristics of Silurian in Kongquehe Slope and Hydrocarbon Distribution Law

Prediction of the Ordovician and Silurian Reservoirs within Baxtopu Fracture Belt in Tarim Basin

Paleohydrocarbon Water Contact Restoration of Typical Silurian Oil and Gas Reservoirs in the Northern Tarim Basin

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

A Counting Method of the Structure Steadying Point in the Silurian of Tarim Basin

Characteristics and distribution of depositional systems of Silurian in Tarim basin

Lower Silurian graptolites from southern Anhui

Hydrocarbon Filling Ages and Evolution ofthe Silurian Asphalt Sandstones in Tarim Basin

A New Ordovician-Silurian Boundary Section in Guizhou, South China

Discussion on exploration direction and depositional system of Silurian-Devonian in Tarim Basin, China

Study on Oil-gas Accumulating Conditions in Silurian of Abei-Shunbei Block

Distribution of the Silurian shale in China