Jurassic Coal-bearing Strata and Coal-forming Patterns in the Yining Basin;

Analysis of Red Beds in Yining Basin and Coal Looking Orientation

The simulation results of Jurassic coal-measures in Yining Basin, Xinjiang show that when simulation temperature is 380 - 420℃ , hyrocarbon generation reaches its peak stage, and hydrocarbon generation stops at the temperature 450 - 500℃ To compare with lipti.

Structure and fluid evolution of Yili basin and their relation to sandstone type uranium mineralization;

Influences of Zhahe fault on hydrogeological conditions of deposit No.511 at the southern margin of Yili Basin;

Geological characteristics and metallogenic mechanism of No. 511 sandstone-type uranium ore deposit in Yili basin,Xinjiang;

Lots of subaqueous gravity flow sedimentary bodies were developed in the Eocene strata of Chaluhe Fault Depression,the Yitong Basin.

The Caluhe Depression of the Yitong Basin is a extension rift basin,due to the complex tectonics,particular morphology,sedimentary source from several directions,several depocenter and subsidence center and the rapid facies transition,there is much difficulty in the stratigraphic division and correlation.

Characteristics and Hydrocarbon Generation-Expulsion Histories of Source Rocks in Moliqing Rift of Yitong Basin;

Diagenesis of reservoir of the Shuangyang Formation of Paleogene in Moliqing Faulted Depression of Yitong Basin, Jilin Province;

Study of Eocene lithologic traps in Chaluhe fault depression of Yitong Basin;

REE geochemistry of sandstone-type uranium deposit in interlayer oxidation zone in the southern margin of Ili Basin,Xinjiang;

Super-enriching Mechanism of Disperse-elements Re and Se in Interlayer Oxidation——A Case Study of the Zhajistan Interlayer Oxidation Zone Sandstone-type Uranium Deposit, Ili Basin, Xinjiang;

Depositional system of the Lower-Middle Jurassic Shuixigou Group in the western segment of the southern margin of the Ili basin and its controls on uranium mineralization;

The main purpose of this paper is to study the general character and the difference of three sets of soluble organic matter from Jurassic, Cretaceous and Tertiary of Kashan area in Iran Basin.