Fig. 11
From: Assessment of lithium potential for future exploration in the Ghahavand Plain of Western Iran
(a) Plot of Sr/Cu versus Ga/Rb 70,73, of the Ghahavand Plain sediments, showing that the sediments were deposited under cold-dry conditions. (b) Diagram of A-CN-K 79,80. Most of the Ghahavand Plain sediment samples plot above the plagioclase–K-feldspar line, showing weak to intermediate weathering (weathering line and mixing sediment linr from Srivastava et al.,81 and K-metasomism line from Fang et al., 82).
