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Minerals 2021, 11, 1330 19 of 23 Minerals 2021, 11, 1330 20 of 24 deionized water (Figure 18), indicating that high-salinity fluid is the main migration carrier of ore-forming elements. Figure 18. Diagram of K and Li element content in distilled water and NaCl solution over temperature in water–rock re- Figure 18. Diagram of K and Li element content in distilled water and NaCl solution over temperature in 5.3.5. Geotectonics eruptions, and metallogenic accumulations in Central China and South China [57]. 2 rJoiacnkgblienltgsedxetpernedssiniognt,owthitehNaNdEi.stAricbcuotridoingarteoathoefr3e5s2e7arckhmre(sFuilgtusroefX4)u,eatccaol.u(n2t0in15g)f[o54r], vnoelacralnyichaclftiovfittyhienwtheoPlealdeeopgreensesiwona,samnadinalnyadvisetraibguettehdiciknnthesesNoEf-mtroenreditnhganSo2n0g0limaofrPolamin, NthoertShaCshinFaoPrmlaianti,oandtoJiQainagnhjiangPlFaoinrm.Tathioenth[i3c5k,e5s8t].bSaosmaltewbasamltosraemtphlaens1c0o0ll0ecmtedthinck, athnedBthaleinmgsahgamnaawreasamreatiynplyicathlothleoilietiictebsaosaflctoicnmtinaegnmtaal,rwifthtiychpew, washoicnhlyarseproircahdiincaKll,yLei,x- pRobs,eSdr,oZnn,thCeus, uanrfdacoet.heFrreolmemtehnetsC[r5e9t]a.ceous to the Paleocene, a large-scale lithospheric extenMsionstcshcahroalcatresribzeldiebvye vthoalctatnhiec acoctmivpitoys,itrioftnboafsimn afogrmaatiisomn,aaindlylacorgnet-rsocllaelde mbyintehreal- iczoamtiopnosoitcicounrorefdthiensNouorcthe rCehginoan,[a3n2,d55a,s5t6h]e.nAotspthersea–mliethtoimspeh,edrueeinttoertahcetieoxntsenlesaiodntofththee lhitehtoersopghenre,ityheirnetwheresoaulsrocelareggei-osnca.lTehfaoulelitietdicbbaassinalst,svaorlecatnhiecerreusuplttioonfs,aarnedlamtivetealyllohgiegnhic adcecgurmeeuolaftmioenlstiningCaet nthtreaslhCahllionwa apnadrtSoofuththe Clithhinosap[h5e7r]i.c mantle or asthenospheric mantle [60,6V1]o.lcInantriaccoronctiknsenatraelwthiodleliyitidcibstarsiablutstegdeninertahlleyJhianvgehhainghBabsoinro,nwciothntaenttost,arlaanrgeiangof 2 Most scholars believe that the composition of magma is mainly controlled by the c5o.3m.6p.oPsailteiocnenoefPthaeleosocluimrcaetereagnidonP,aalenod-LaskteheCnoomsphoesirteio–nlithosphereinteractionsleadto action. water–rock reaction. Compared with leaching results under normal temperatures and the chemical analysis resultAscocfoJridaningghatonGbausainb[5ri1n]e,M(Teasbolezo4i)c,tvhoelcdainssicolruotcioknsoinfLeai,sKte,rSnr,CMhign,anadreodthiveirdeldeminetnots ifnouarurtocklabveltws eaxtetern–rdoinckg troeathcteioNnNs Eis. Asicgcnoirfidcianngtltyo thieghresreathrcahnrtehseulntsoormf Xaul teetmalp. e(2r0a1tu5)re i[m54m],evrsoilocnanriecsualcttsi,vbituytisntillthtweoPaolredoegresnoefwmasgnmitauidnleylodwisetritbhuatnedthienetlhemeeNnEt-ctorenntednintgin tShoenbgalisaion Pblrainine, NinodritchatCinhgintahaPtlahiing,hantedmJipaenrgahtuarnePs larien.mTohretfhaivcokreasbt lbeafsoarltKw, aLsi,mNoar,eatnhdanSr e1n0r0i0chmtehnictk.,Tahnedprtohceesmsawgimthahwigahserm-tahiannly-ntohromleaiilttiecmbpasearlattiucrmesahgamsaa,swighnicifihcawnatsimonplayct osnpotrhaediccoamllypoexsiptioosnedoofnfluthide,swurhfaiche.iFsrfoamvotrhaebClerefotarceigonuesotuosthroecPkasletocreenaec,taalnadrgpe-rsocvaildee mlitahtoesrpiahlesroicurecxetefonrsibonrinceh.aWraacteri–zreodckbryeavctoilocnanoicf igacnteivoiutys,roricfkt ibsaosnine ofofrtmheatimonp,oartnadnt plarrogce-ssceaslefomrtihnermalinzaetriaolnizaotcicounrroefdlitihniuNmor–tphoCtahsisniuam[3-2ri,5ch5,5b6r]in.eA,tatnhdesuarmfaecetimevea,pdouraettion athned ceoxntecnesnitornatiofntahre ltihtheomspahinerme,ecthaerneismwesrfeoratlhsoe mlairnger-ascliazlaetifoanulotfedbribnaes.ins, volcanic 5.3.5. Geotectonics Volcanic rocks are widely distributed in the Jianghan Basin, with a total area of 5049 km2,AaccorudnintigngtofGorua1n8%[51o],fMtheesobzaosiicnvoarlcean.iVcroolcaknsiicnreoacsktesrnarCehwineallardeedvievliodpeedinintotfhoeur 2 5fr0o4m9k0m.48,a×c1c0ountotin1g7.f8o×r180%[o6f2]t.hAesbasisnolaurbelae.eVloemlcaenitc, brocrkosnacraenwbellrdelevaesleodpiendlianrgthee −6 −6 Jqiaunagnltiintigesdienptroessuirofna,cewhitohtaspdriisntrgisb,uctoionnceanrteratoefd35b2ri7nkems, an(Fdigmuerete4o)r,icacwcoautenrt.inAglofnogr nweiatrhly hthaelfolafrtghee-swcahloelevodlecparneiscsieornu,patniodnainatvheeraPgaelethoicceknneesinsotfhmeoJiraentghlaing20d0epmrefsrsoimont,haeSlahragsehi FnourmbaetironoftoboQrioan-jciaongtaFinoirnmgamtioine[r3a5l,s58c]a.rSrioemdebbyamsaaltgsmamapalnedscpoollsetc-stetadgienhthyedrBoatlhinegrmshaaln aflrueaidasrceotuylpdichaalvtheopleroiivteidseodf caolnatrignentuaml rbifetrtyopf eo,rwe-fhoicrmh ainregrmicahteinriaKls, Lfoi,rRbbr,inSer,dZenp,oCsuit,saind oththeeJriaenlegmlinegntdse[p5r9e].ssion. the heterogeneity in the source region. Tholeiitic basalts are the result of a relatively The sedimentary environment of Paleocene salt-bearing strata in the Jiangling de- high degree of melting at the shallow part of the lithospheric mantle or asthenospheric pression was dominated by a warm and dry environment, which alternated frequently mantle [60,61]. Intracontinental tholeiitic basalts generally have high boron contents, with a humid environment. Under the paleogeomorphic background of “high mountain ranging from 0.48 × 10−6 to 17.8 × 10−6 [62]. As a soluble element, boron can be released and deep basins”, the brine in the lake basin reached sodium chloride saturation through in large quantities into surface hot springs, concentrated brines, and meteoric water. Along strong evaporation (extremely dry and hot climate events), and halite precipitated. The with the large-scale volcanic eruption in the Paleocene in the Jiangling depression, a large brines continued to be evaporated to form boron-rich brines, and with the length of salt-forming time, halite layers with different thicknesses formed. The Paleocene–Eocene salt-bearing strata in the Jiangling depression are characterized by mineral deposits suchPDF Image | Origin of Lithium Potassium Rich Brines in the Jianghan
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