ECONOMIC GEOLOGY AND THE BULLETIN OF THE SOCIETY OF ECONOMIC GEOLOGISTS, 1998 MAY, V93 N3



   8.1 Allibone, AH; Windh, J; Etheridge, MA; Burton, D; and others.
         Timing relationships and structural controls on the
       location of Au-Cu mineralization at the Boddington gold
       mine, Western Australia.                                     pp. 245-270
   8.2 Hagemann, SG; Brown, PE; Ridley, J; Stern, P; and others.
         Ore petrology, chemistry, and timing of electrum in the
       archean hypozonal transvaal lode gold deposit, Western
       Australia.                                                   pp. 271-291
   8.3 Brauhart, CW; Groves, DI; Morant, P.
         Regional alteration systems associated with volcanogenic
       massive sulfide mineralization at Panorama, Pilbara, Western
       Australia.                                                   pp. 292-302
   8.4 Shimizu, T; Matsueda, H; Ishiyama, D; Matsubaya, O.
         Genesis of epithermal Au-Ag mineralization of the Koryu
       mine, Hokkaido, Japan.                                       pp. 303-325
   8.5 Clark, AH; Archibald, DA; Lee, AW; Farrar, E; and others.
         Laser probe Ar-40/Ar-39 ages of early- and late-stage
       alteration assemblages, Rosario porphyry copper-molybdenun
       deposit, Collahuasi district, I region, Chile.               pp. 326-337
   8.6 Vikre, PG.
         Quartz-Alunite alteration in the western part of the
       Virginia Range, Washoe and Storey Counties, Nevada.          pp. 338-346
   8.7 Leach, DL; Hofstra, AH; Church, SE; Snee, LW; and others.
         Evidence for proterozoic and late Cretaceous-early
       tertiary ore-forming events in the Coeur d'Alene district,
       Idaho and Montana.                                           pp. 347-359
   8.8 Roberts, S; Sanderson, DJ; Gumiel, P.
         Fractal analysis of Sn-W mineralization from Central
       Iberia: Insights into the role of fracture connectivity in
       the formation of an ore deposit.                             pp. 360-365