All Stories

  1. Sulfur Isotopic Composition of Gypsum from Paleocene, Northwest China: Implications for the Evolution of Eastern Paratethys Seawater
  2. Origin of paratacamite in the Kuqa Basin, Xinjiang, China: Defined by Cu isotope values
  3. Marine transgressive–regressive cycles and evolution on ancient salt lake in the northwestern Tarim Basin in the Paleocene, Xinjiang Province, China
  4. A Rapid Marine Regression in the Southwestern Tarim Basin in the Latest Cretaceous: Comparison of Two Different Evaporitic Sequences in the Yarkand Basin, Xinjiang Province, China
  5. A Rapid Cu Enrichment Mechanism from Cu-Bearing Brine in Kuqa Basin, Xinjiang, China: Controlled by Crystallized Sequence of Saline Minerals
  6. Whether the Middle Eocene Salt-Forming Brine in the Kuqa Basin Reached the Potash-Forming Stage: Quantitative Evidence from Halite Fluid Inclusions
  7. 库车盆地早始新世成盐期卤水温度及其意义
  8. The History of Transgressions during the Late Paleocene-Early Eocene in the Kuqa Depression, Tarim Basin: Constraints from C-O-S-Sr Isotopic Geochemistry
  9. The Mesozoic-Cenozoic tectonic settings, paleogeography and evaporitic sedimentation of Tethyan blocks within China: Implications for potash formation
  10. Quantitative temperature recovery from middle Eocene halite fluid inclusions in the easternmost Tethys realm
  11. Paratacamite from Gypsum Veins in Sandstones of the Kuqa Basin, Xinjiang, China: Implications for a New Epigenetic Cu Enrichment Mechanism
  12. Discussion on the Scenario of Salt Accumulation in Yarkand Basin during Late Cretaceous
  13. Fault Zone Fluid Deep-penetrating Techniques for Potash Deposit Prediction in Lanping-Simao Basin, Yunnan, South China
  14. Spatial Distribution of Halite in Kuqa Basin from Paleogene to Neogene and Signification of Potash Survey
  15. The Formation Model for Marine Potash Deposits within China's Small Continental Blocks
  16. Hydrochemical characteristics and controlling factors for waters’ chemical composition in the Tarim Basin, Western China
  17. Discovery, Genesis and Significance of Metallic Minerals in Evaporate Series in the Kuqa Basin