地质通报
地質通報
지질통보
GEOLOGICAL BULLETIN OF CHINA
2014年
5期
741-750
,共10页
胡小梅%龚鹏%李娟%闭向阳
鬍小梅%龔鵬%李娟%閉嚮暘
호소매%공붕%리연%폐향양
石门寺钨铜矿%风化作用%W%Cu成矿元素%表生地球化学行为
石門寺鎢銅礦%風化作用%W%Cu成礦元素%錶生地毬化學行為
석문사오동광%풍화작용%W%Cu성광원소%표생지구화학행위
Shimensi tungsten-copper mining area%weathering%tungsten-copper metallogenic elements%supergene geochemical behavior
以江西省武宁县石门寺钨铜矿区燕山期和晋宁期岩体风化作用过程中W、Cu等元素的表生地球化学行为为研究对象,通过反映风化程度的化学风化指数CIA、风化作用过程中组分得失的估算、不同介质中W、Cu等成矿元素的含量变化及大离子亲石元素表生地球化学行为等方法的研究表明,石门寺钨铜矿区2个时期岩体元素淋失与风化强度有关,土壤剖面中碱金属、碱土金属元素大量淋失,而W、Cu等成矿元素在土壤B层中显著富集;从岩石到土壤、再到水系沉积物风化过程中,W、Cu等成矿元素含量逐渐升高,为此,一级水系沉积物和B层土壤是赣北九岭W、Sn、Cu、Mo多金属矿集区地球化学找矿的绝佳采样介质,是矿集区内找矿新突破的有效手段。
以江西省武寧縣石門寺鎢銅礦區燕山期和晉寧期巖體風化作用過程中W、Cu等元素的錶生地毬化學行為為研究對象,通過反映風化程度的化學風化指數CIA、風化作用過程中組分得失的估算、不同介質中W、Cu等成礦元素的含量變化及大離子親石元素錶生地毬化學行為等方法的研究錶明,石門寺鎢銅礦區2箇時期巖體元素淋失與風化彊度有關,土壤剖麵中堿金屬、堿土金屬元素大量淋失,而W、Cu等成礦元素在土壤B層中顯著富集;從巖石到土壤、再到水繫沉積物風化過程中,W、Cu等成礦元素含量逐漸升高,為此,一級水繫沉積物和B層土壤是贛北九嶺W、Sn、Cu、Mo多金屬礦集區地毬化學找礦的絕佳採樣介質,是礦集區內找礦新突破的有效手段。
이강서성무저현석문사오동광구연산기화진저기암체풍화작용과정중W、Cu등원소적표생지구화학행위위연구대상,통과반영풍화정도적화학풍화지수CIA、풍화작용과정중조분득실적고산、불동개질중W、Cu등성광원소적함량변화급대리자친석원소표생지구화학행위등방법적연구표명,석문사오동광구2개시기암체원소림실여풍화강도유관,토양부면중감금속、감토금속원소대량림실,이W、Cu등성광원소재토양B층중현저부집;종암석도토양、재도수계침적물풍화과정중,W、Cu등성광원소함량축점승고,위차,일급수계침적물화B층토양시공북구령W、Sn、Cu、Mo다금속광집구지구화학조광적절가채양개질,시광집구내조광신돌파적유효수단。
Taking the supergene geochemical behavior of such elements as Cu and W in Yanshan period and Jinning period of rocks during the process of weathering as the study object, the authors conducted the investigation, and the results can offer an effective geochemical basis for the development of regional geochemical prospecting and the establishment of geological-geochemical pros-pecting model for the magmatic hydrothermal type tungsten-copper deposit. Through the study of CIA that reflects the weathering degree, the estimation of components of gain and loss in the process of weathering, the content changes of such ore-forming ele-ments as tungsten and copper in different media, and the supergene geochemical behavior of the large ion lithophile elements, the au-thors have reached some conclusions:The elements leaching of the two periods of rocks is related to the intensity of the weathering in the Shimensi tungsten-copper mining area. The alkali metals and the alkali-earth metal elements have been subjected to consider-able leaching in the soil profile whereas W, Cu and some other ore-forming elements are significantly concentrated in soil horizon B. W, Cu and some other ore-forming elements gradually increase in the process of weathering from rock to soil and then to the stream sediments. Therefore, excellent sampling media seem to be the first-order stream sediments and soil horizon B for geochemical pros-pecting in the Jiuling W, Sn, Cu and Mo polymetallic ore concentration area in northern Jiangxi Province. These effective prospect-ing means can make a new breakthrough in the ore concentration area.