富金斑岩型铜矿床基本特征、成矿物质来源与成矿高氧化岩浆-流体演化

《富金斑岩型铜矿床基本特征、成矿物质来源与成矿高氧化岩浆-流体演化》由会员上传分享，免费在线阅读，更多相关内容在行业资料-天天文库。

1、4555<5897X6559X566（5R）<59TU6>49==86+8=93#73*’+758#696839?6483*’+8@9<@#’;=694833839:5#;59A#+*7#9’B*;B**’+968!:96B#’;:/?:=?/@=@>:??-=0-?:A%BA:CD-&:E:%>(=-0:F%&(&B;@)-&-=(B-0%&A2G

3、02>B%:&<=-;(B-0H:;>(&:?;2B:&%>(=>A(&0>:&B%&-&B(;F(=)%&(=>(B>:&H-=)-&B?;(B-G:2&0(=%-AI3:AB:CB/:A-:;0-=0-?:A%BA(??-(=B::>>2=%&%A;(&0<(=>B-==(&-A(>>=-B-0B:>:&B%&-&B(;F(=)%&AIJ/-?:=?/@=@AB:>KAA?(&(=(&)-:C>:F?:A%B%:&A，C=:F;:L,>(;><(;K(;%&-0%:=%B-，M2(=BE0%:=%B-(&0B:&(;%B-，B/=:2)//%)/,>(;><(;K(;

4、%&-M2(=BEF:&E:&%B-，B:(;K(;%&-F:&E:&%B-(&0A@-&%B-；(&0>:FF:&;@-F?;(>-0(BA/(;;:L>=2AB(;;-H-;（4N6KF）(&0，/-&>-，(=-;%K-;@B:G-(AA:>%(B-0L%B/>:-H(;H:;>(&%>=:>KAIO&0/@0=:B/-=F(;G=->>%(A(=->:FF:&;@(AA:>%(B-0L%B/):;0<=%>/?:=?/@=@0-?:A%BAIP%QG=:(0(;B-=(B%:&B@?-A(=-%0-&B%C%-0%&B/-A-0-?:A%BA，C=:F-(=;@B

5、:;(B-%&B%F-，%&>;20%&)D(<+(A%;%>(B-(;B-=(B%:&，?:B(AA%>A%;%>(B-(;B-=(B%:&，?=:?@;%B%>(;B-=(B%:&，%&B-=F-0%(B-(=)%;;%>(;B-=(B%:&，A-=%>%B%>（?/@;;%>）(;B-=(B%:&(&0(0H(&>-0(=)%;;%>(;B-=(B%:&，(&0(0H(&>-0(=)%;;%>(;B-=(B%:&:>>2==-0%&B/-A(F-B%F-(A,%C%>(B%:&I3:AB:C):;0%A%&B=:02>-0L

6、%B/>:??-=02=%&)?:B(AA%>A%;%>(B-(;B-=(B%:&AB()-，(&0):;0>:&B-&BA(;A:>:==-;(B-L-;;L%B/B/-%&B-&A%B@:COB@?-M2(=BEH-%&;-BAI3(&@):;0<=%>/?:=?/@=@>:??-=0-?:A%BA(=-0-C%>%-&B%&F:;@G0-&2F，=%>/%&?;(B%&2F)=:2?-;-F-&BA，-A?->%(;;@=%>/%&?(;;(0%2F(&0?;(B%&2FIJ/-K-@>:&B=:;;%&)?=:>-AA-A:&):;0<=%>/?:=?/@=@>:

7、??-=0-?:A%BA%&>;20-：（4）A:2=>-=%>/%&:=-/(&%AFC:=D2，O2(&0:B/-=F%&-=(;%E(B%:&-;-F-&BA-CC%>%-&BF:H-%&B:F()F(F-;B，（R）D2，O2(&0:B/-=:=--AA-A:CF()F(-H:;2B%:&，（S）F()F(B%>H:;(B%;--CC%>%-&B;@-A>(?-AC=:FF()F(，(&0B/-