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Minerals 2021, 11, 1330 4 of 23 Minerals 2021, 11, 1330 4 of 24 Figure 1. (A) Distribution of major Mesozoic–Cenozoic basins in China and location of Jianghan basin. BB, Baise Basin; Figure 1. (A) Distribution of major Mesozoic–Cenozoic basins in China and location of Jianghan basin. BB, Baise Basin; BGB, Baidu Gulf Basin; BHG, Bohai Gulf Basin; CQB, Cuoqing Basin; CXB, Chuxiong Basin; DHB, Dunhuang Basin; ELB, BGB, Baidu Gulf Basin; BHG, Bohai Gulf Basin; CQB, Cuoqing Basin; CXB, Chuxiong Basin; DHB, Dunhuang Basin; ELB, Erlian Basin; HLB, Hailaer Basin; JGB, Junggar Basin; JHB, Jianghan Basin; LSB, Lanping–Simao Basin; MHB, Mehe Basin; Erlian Basin; HLB, Hailaer Basin; JGB, Junggar Basin; JHB, Jianghan Basin; LSB, Lanping–Simao Basin; MHB, Mehe Basin; ODB, Ordos Basin; QB, Qaidam Basin; QTB, Qiangtang Basin; SCB, Sichuan Basin; SJB, Sanjiang Basin; SLB, Songliao ODB, Ordos Basin; QB, Qaidam Basin; QTB, Qiangtang Basin; SCB, Sichuan Basin; SJB, Sanjiang Basin; SLB, Songliao Basin; Basin; SNCB, Southern North China Basin; SSB, Sanshui Basin; SYSB, South Yellow Sea Basin; TB, Tarim Basin; THB, SNCB, Southern North China Basin; SSB, Sanshui Basin; SYSB, South Yellow Sea Basin; TB, Tarim Basin; THB, Turpan–Hami Turpan–Hami Basin; YEB, Yingen–Ejinaqi Basin. (B) DEM map showing the location of the Jiangling depression (diago- Basin; YEB, Yingen–Ejinaqi Basin. (B) DEM map showing the location of the Jiangling depression (diagonal white solid nal white solid lines) in the Jianghan Basin (white dashed lines). The red lines show the major faults surrounding the ba- sline.sG)einoltohgeicJialndgahtanfrBoamsin[4(0w].hitedashedlines).Theredlinesshowthemajorfaultssurroundingthebasin.Geologicaldata from [40]. The Jianghan Basin is surrounded by high mountains that are 1000~3000 m above The Jianghan Basin is surrounded by high mountains that are 1000~3000 m above sea level. Its periphery is surrounded by low hills with a height of more than 120 m, and sea level. Its periphery is surrounded by low hills with a height of more than 120 m, the central area is a large plains area [41]. The interior of the basin is covered by Quater- and the central area is a large plains area [41]. The interior of the basin is covered by nary sediments, and the lower strata are exposed only at the edge of the basin (Figure Quaternary sediments, and the lower strata are exposed only at the edge of the basin 2A). The Yangtze River flows from the northwest to the southeast and then to the (Figure 2A). The Yangtze River flows from the northwest to the southeast and then to the northeast (Figure 2B). There is hot-spring activity in the Songzi area of the basin. The northeast (Figure 2B). There is hot-spring activity in the Songzi area of the basin. The Jianghan Basin is composed of Neoproterozoic to Middle Triassic marine carbonate rocks Jianghan Basin is composed of Neoproterozoic to Middle Triassic marine carbonate rocks and continental shelf clastic rocks, Late Triassic to Early Cretaceous continental clastic and continental shelf clastic rocks, Late Triassic to Early Cretaceous continental clastic rocks, and a large number of Late Cretaceous to Paleocene evaporite rocks and a clastic rocks, and a large number of Late Cretaceous to Paleocene evaporite rocks and a clastic rock series interbedded with basalt (Figure 2C). rock series interbedded with basalt (Figure 2C).PDF Image | Origin of Lithium Potassium Rich Brines in the Jianghan
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