Page 215 - Caldera Volcanism Analysis, Modelling and Response
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190                                                        W.U. Mueller et al.





             locus   during  feldspar–  associated  edifice  tuff  lapilli  origin;  syneruptive  Transport  low-  currents.  as  deposits  sedimentation  through  represents  fluids  subaqueous  caldera

             and     dykes-sills  are  suites.  crustal-thinning  volcanic  and  pyroclastic  and  settling  hydrothermal  Locus:  and
             process  of  construction;  dykes  plutonic  and  of  part  tuff  in  and  reworking.  high  density  suspension  background  fines  Iron-formation  of  floor  faults


             Interpretation,  Intrusion  (c)  edifice  quartz-phyric  late  with  Extension  processes.  central  Locus:  Pumice  (b-1)  indicates  beds  primary  both  limited  with  mechanism:  concentration  Mudstone:  pelagic  vitric  and  water  (b-2)  percolation  diagenesis.  and  intracaldera  margin






                     mafic     dyke-sill  late  to  T ad ,  of  angular  pumice,  crystals;  black  is  vitric  in  folded  (silicified
             volcanic  sills;  contemporaneous  related  lithofacies:  2–50 cm-thick  turbidites  T abc ,  composed  turbidites  felsic  beds  lithofacies:  chert  chert–  jasper–magnetite


             of  rocks  porphyritic  and  construction  phases  with  tuff  T ab ,  beds  and  vitric  fragments,  euhedral  silicified)  tuff  fine-grained  mudstone  iron-formation  of  units  tuff)–jasper,  m-thick  as  chert  carbonate
             Salient characteristics  volcaniclastic  to Aphanitic  dykes  felsic,  are intrusions  caldera  with  feldspar–quartz-phyric  o2,706 Ma)  (FQP  pluton Poularies  Volcaniclastic  2–20 m-thick  lapilli  and  and (Ta-S 3 beds);  T abcde  wispy  shards,  volcanic  lithic  and  broken  (locally cm-thick  capping mudstone  probably  M-thick  tuff.  cap (silicified

                                            beds




         Caldera.  and  (c)  and  Late  (b-1)  tuff  and           (b-2)



         Mine                           iron-  lithofacies

         Hunter      dykes              and

         of  Lithofacies/lithology  and  Sills  Volcaniclastic  lithofacies  formation
         lithofacies  (c)            (b)




         volcanic  stage  2nd  event    2,740.8 Ma)  felsic  and  than  as documented  dykes aphanitic  yield  dykes


         Subaqueous  caldera  mine  formational  0.5–2 km-thick:  subsidence  2,728–2,730 Ma  (inheritance  dykes  on  units.  flow  dykes  older  oldest  not  did  age  for  determinations,  Phenocryst-rich  o2,730 Ma





         1   Hunter  stratigraphy  caldera  Age:  Based  lava  No  2,730 Ma  the  phases  zircons
         Table     Upper
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