Bacteriogenic and magmatic S sources in the Cabildo

Download PDF
0 downloads 0 Views 40KB Size Report
Comment
range of sulphides from the MoYbearing skarn zone differs from the rest of the skarn showing more depleted values (Y8.6 to Y5.6Å). A twoYstage mineralization ...


      

                 !"#$%&' ( ")) *#' * )* #+' ! , / ! ( -.  %

  0 1  !2 # 3  *2  4&25 3 6789  7  :7 ; # 3  *2  4 4;6787?9 @  ;2A 7 489 2 '      7 

7   ' 3   3  8  4 8   3   2   ; 3 2 8   B%C9 , 2      (7   )D  7 3   ; ?     8 ,       4 +E+F*G 8 HE//FI9  7 J7   @  ;2A

7 489  7 49 ? 2  K   , į+* 8    @  ;2A 72   K  ; D  4 +L  M %NO9 "   '   7 ? 72     8  3;  87 4 +  %/O9 PD3'  į+* 8  72      8 ? Q        ? D 8  2  37 4 LN  /NO9  D  8  Q  2  @  ;2A 2   225 %9 -  8  2;    7 8  ;  8   8     ;   9 *    Q   7 27   D   2  3    27   2;   , ?    7  3           Q  3   @  ;2A 2  , * 7  7 ?  Q     ; 8    '    7     8  *      ? Q  22  ?; *722 8   ;2  ' 7   2  ;  LH *=LN*'   D D   7   8  7    ' D 8   2  7  4D      D    8  2; 9  8   7 ' D 

      2   8 7 4 79     ? B%C ?3 0 $  49 PGC Publishing, Adelaide' %L/ /

                ,,"%' " "$%' 1 ","'%' ) ",,+'%'  !F,"'% !  *"% %

" 3   73 ' 2 4  63 83 9 ! 2 *  ,' # 3 R  1  + ! 2 *  :  ' # 3 R  2 S:  ""F  ! 2 *  ,' # 3 R  2 S:  ""F 



I 2   8 8   3  ;    '   7 8    3      2 , "    ;  3    ; ; 2 8 8'    3    3   ' D  78 27 7  D   7       K  , 2 ;    *7  " ;   2 D       2  ;  3 3    8 ?   7   7  "   3' 2 7;    2    !    ' 788    3 27 8  7 ;   7  7            78     7   2       7         7 ' 3  3       2 8  3  2    23  8 ;2   33 8  77      7     ; 8 28 '  87      , D 2   8 8 788   3    S F J7  2   7    2   ' 2 8  8         88   7 7'  3    2  !2  7   2K ;' 8  7K     7   ;2     7        3  7     8