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Minerals 2021, 11, 1330 5 of 23 Minerals 2021, 11, 1330 5 of 24 Figure 2. (A) Geographic location of the Jianghan Basin (modified from [41]); (B) locations of sampling boreholes; (C) Figure 2. (A) Geographic location of the Jianghan Basin (modified from [41]); (B) locations of sampling boreholes; 22 westernJJiianghaanBBaasisninthtahtactocvoevresrasnaanreaareoaf noefanrleyar6l5y0065k0m0 k. Vmol.caVnoiclcraoncikcsrcoocvkesrcmovoreer tmhaonrehtahlfaonfhthaelfdoefptrheessdioenp,raenssdiothne, aQnidngtsheuQikionugsfahulitk, oJiushfanuslit,faJuislht,aWnseinf’aunlsti, fWauelnt,’ansdi Gfaounltg,’and–SGonognzgi’afanu–lStoanregzloi cfauteldt artethloeceadtegde aotf the eddepgereosfsitohne, dwehpircehssjoioint,lywchoinchtrojolsintthlye fcornmtraotlisonthaenfdoremvaotliuotnioandofetvhoeludteiopnreosfsitohne.dTehpereWssaionnc.hTenhge Wfauanltcihnenthgefamuildtdinlethoef mthieddele- porfetshseiodnedpirveisdseiosnthdeivdiedpersesthsieondeinptroestswionpianrtos.tAwolaprgaertns.umAbleargoef bnausmalbtseraroefdbiasstrailbtsutaerde idnistthreibnuotretdheinastheernnJoiartnhgelainstgerdnepJiraensgsiloing(Fdiegpuress3iAon). (TFhigeuarea3Ain).wThiechartehae ibnaswahlticishdthise- basin-filling evolution and stratigraphic column of the Jianghan Basin (modified from [42,43]). (C) basin-filling evolution and stratigraphic column of the Jianghan Basin (modified from [42,43]). The Jiangling depressiion iis a Late Cretaceous to Paleogene riifftt basiin iin the soutth-- basalt is distributed in the Jiangling depression reaches 3570 km2, and the basalt has a large tributed in the Jiangling depression reaches 3570 km2, and the basalt has a large accu- accumulative thickness, with a maximum thickness of 588.6 m. The horizontal distribution mulative thickness, with a maximum thickness of 588.6 m. The horizontal distribution and scale of the volcanic rock are controlled by the period and intensity of fault activity. and scale of the volcanic rock are controlled by the period and intensity of fault activity. At the same time, the distribution of basalt is controlled by the nearly east–west-oriented At the same time, the distribution of basalt is controlled by the nearly east–west-oriented fault [9]. A large number of granites are distributed in the southeastern Jiangling depres- fault [9]. A large number of granites are distributed in the southeastern Jiangling de- sion. In the southeastern Jiangling depression, the granite distribution area can reach pression. In the southeastern Jiangling depression, the granite distribution area can reach 2 1600km2 onTaohuashanintheHuarongarea(Figure3B).Thetypicalgranitesaremainly 1600km onTaohuashanintheHuarongarea(Figure3B).Thetypicalgranitesaremainly gneiss-like biotite monzonite, medium- to fine-grained biotite monzonite, medium-grained gneiss-like biotite monzonite, medium- to fine-grained biotite monzonite, medi- porphyritic biotite monzonite, and granitic pegmatite, which formed at 129 Ma in the Early um-grained porphyritic biotite monzonite, and granitic pegmatite, which formed at 129 Cretaceous [44]. These granites may have been the source of lithium in the brine [30]. Ma in the Early Cretaceous [44]. These granites may have been the source of lithium in The brine-type lithium and potassium deposits spatially intersect with basalts and the brine [30]. granites. Therefore, it is speculated that the mineralization of the brine deposits may be affected by a deep source of materials [45,46].PDF Image | Origin of Lithium Potassium Rich Brines in the Jianghan
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