论文信息 - The Seismic Response Characteristics of Polyhalite with Shaded Potash Mine in Central Sichuan - 字舞流文

The Seismic Response Characteristics of Polyhalite with Shaded Potash Mine in Central Sichuan

Potash deposition is the result of final phase of brine sedimentary evolution,it’s a limited distribution and easily soluble mineral,it is difficult to find the features on the ground,therefore the prospecting is extremely tough.

M. Li | Xiang Xu | Yan Zhang | Da Peng | Feng Ding | Wei Liu

[1] C. Ayora,et al. Evidence of potash salt formation in the Pliocene Sedom Lagoon (Dead Sea Rift, Israel) , 2009 .

[2] H. Rahimpour-Bonab,et al. Origin of secondary potash deposits; a case from Miocene evaporites of NW Central Iran , 2005 .

[3] Liu Cheng. Sedimentation of glauberite and its effect on potash deposits formation in Lop Nur salt lake, Xinjiang,China , 2007 .

[4] P. Nelson. Evaluation of Potash Grade with Gamma-ray Logs , 2007 .

[5] Sun Guo-fang. Brine geochemistry and prediction of potash formation at salt occurrences in the western Tarim basin , 2007 .

[6] Ma Wan-dong. Geochemical Characteristics on Brine and Potash Perspective in the Western Tarim Basin , 2006 .

[7] D. Timko. Potash Evaluation Using Well Logs , 1964 .