J4 ›› 2015, Vol. 21 ›› Issue (2): 177-.
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ZHANG Liangju,HU Huiyi,ZENG Weilai,LI Dongsheng,ZENG Nanshi, RUAN Qingfeng,SONG Chuxin,QIN Minfeng
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Abstract:
Quartz,bitumem,prehniteandCu-bearingmineralswidelyoccurinamygdaloidbasalticdrusefromPugecounty,south Sichuan. According to their occurrences and relationships, three types of basaltic druse are divided: quartz-bitumen druse, rock crystal-bitumendruse,rockcrystal-prehnitedruse.Themineralassemblagesfromrockcrystal-prehnitedrusedisplaythefeatureof nodules, which outward include prismatical rock crystals, prehnite spherulites and Cu-bearing minerals spherulites. Moreover, Cu-bearingmineralsspheruliteshavethefeatureofcirclelayeredstructure,includingnativecopper(core),tenorite(mantle)and chalcostaktite-malachite(crust).Observationsinfieldandundermicroscopeshowthattheshapesandoccurrencesofnativecopper controlthepatternoftheCu-bearingmineralsaggregations.Cu-bearingmineralsspherulitesaremainlydistributedintheconvergences amongtheprehnitespherulites,andthecoreisgranularnativecopper.Cu-bearingmineralsveinsincludestretchnativecopper, tenorite,chalcostaktite,occurinthefracturesofdruses.Thecarbonisotopeandinfraredspectrumsuggestthatasphaltisofbiogenesis andoriginatedfromthecarbonaterocksinPermianstrata(P13).Themineralsinbasalticdrusescrystallizedfromtheorganicfluids,the commonly recognized sequence is chalcedony → quartz + bitumen+ native copper → native copper + prehnite → tenorite → chalcostaktite→malachite→calcite.Thespiralgrowthpatternsofbitumen,homogenizationtemperatureofinclusionsinquartzand therelationshipsbetweenbitumenandnativecopperinrockcrystalindicatethatbitumenformedunderthethermalcrackingoforganic (crudeoil),thetemperatureis290-230℃.Nativecoppercrystallizedunder230-160℃.
Key words: typesofdrus;bitumenandnativecopper;rockcrystalandprehnite;shapeandoccurrences;compositionandinfra-red spectrum;genesis;PugecountyinsouthSichuan
ZHANG Liangju,HU Huiyi,ZENG Weilai,LI Dongsheng,ZENG Nanshi, RUAN Qingfeng,SONG . StudyontheBitumenandCu-bearingMineralSpherulitefrom BasalticDruseinSouthSichuan[J]. J4, 2015, 21(2): 177-.
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URL: https://geology.nju.edu.cn/EN/
https://geology.nju.edu.cn/EN/Y2015/V21/I2/177