All Stories

  1. Types of Fluid Alteration and Developing Mechanism of Deep Marine Carbonate Reservoirs
  2. Paired δ13Ccarb and δ13Corg records of the Ordovician on the Yangtze platform, South China
  3. Sulfur isotope of pyrite response to redox chemistry in OM-enriched shales and implications for components of shale gas
  4. Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin
  5. Fluid environment for preservation of pore spaces in a deep dolomite reservoir
  6. Formation mechanism of deep Cambrian dolomite reservoirs in the Tarim basin, northwestern China
  7. Dissolution-filling mechanism of atmospheric precipitation controlled by both thermodynamics and kinetics
  8. Deep Hydrothermal Altered Dolomite Reservoir in the Tarim Basin Northwestern China
  9. REE Compositions of Lower Ordovician Dolomites in Central and North Tarim Basin, NW China: A Potential REE Proxy for Ancient Seawater
  10. Hydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin
  11. Mesogenetic dissolution of the middle Ordovician limestone in the Tahe oilfield of Tarim basin, NW China
  12. Effects of abnormally high heat stress on petroleum in reservoir
  13. Effect of igneous activity on hydrocarbon source rocks in Jiyang sub-basin, eastern China
  14. REE variation and implication of Ordovician dolomites from Tarim Basin, NW China
  15. HYDROTHERMALLY FLUORITIZED ORDOVICIAN CARBONATES AS RESERVOIR ROCKS IN THE TAZHONG AREA, CENTRALTARIM BASIN, NW CHINA
  16. High-quality hydrocarbon source rock in the Paleogene sequence of the Ping Chau Formation, Hong Kong