摘要
TheSainUsgolddepositisatypicalauriferoussulphidequartzveindepositintheInnerMongolianaridsteppeclimaticregion.Theoxidationzonehasbeencontrolledbythearidcli-matesincethebeginningoftheHolocene.Goldsupergeneevolutionischaracterizedbyenlarge-mentofgoldgrains,complicationofthegoldform,raisingofthegoldgradeandincreaseofthegoldfineness;besides,goldandsilverhavetwoenrichmentpeaksatthesamedepth,whichisinsharpcontrasttotheunimodalenrichmentofgoldandsilverandtheoccurrenceofgoldaboveandsilverbelowinahumidclimaticregion.Sunpumpingisthemaincauseforthebimodalenrichmentofgoldandsilver.Illite2M1isoneofthemaincausesfortheupperenrichmentpeakofgoldandsilver.
出版日期
1997年01月11日(中国期刊网平台首次上网日期,不代表论文的发表时间)