Page 39 - Caldera Volcanism Analysis, Modelling and Response
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Magma  production  rate km 3 y  1  (vol/residence  time)  2   10  5 –4   10  5  2   10  4 –5   10  5  2   10  4 –6   10  5  10  4  1   10  2 –2   10  3  10  3 –4   10  3  10  3 –4   10  3  (2004);  Smith  and  (1990);  Lowe  and


                                       (w/             [C03]                   Brown  Froggatt
               residence   (w/oldest  13 ky  to  peak)  (w/oldest  18 ky  to  peak)  (w/oldest  18 ky  to  peak)  mean=972ky,  50 ky  ca.  [B&F99]  Volumes in dense rock equivalent. b this is taken as the difference  [B&S04],  [F&L90],


               Magma  time b  27 ky  to  Up  up  peak),  (w/youngest  65 ky  to  Up  up  peak),  (w/youngest  50 ky  to  Up  up  peak),  youngest  100 ky  ca.  Bulk  zircon  250 ky  to  Up  240 ky  to  Up  (1999);  (2005);  al.





               Oldest  ages                                            119–340 Ma  [B&S04]  Fletcher  and  et Charlier  [C05],  (2001).


               Zircon U--Pb  (SIMS)  age                        (rims)– 346721 ka  608720 ka  [B&F99]  (cores)  peak 1.18–1.44 Ma,  1.3170.03 Ma  [B&S04]  ¼  Brown [B&F99],  (2003);  al.  et  Wilson  [W01],  (1993);






                 disequilibrium  bulk-rock,  or glass  [C03]  [C03]  6973–7676 ka,  mean=7172ka  sources:  Data  Charlier  [C03],  Wilson


               U--Th  minerals  age         17375 ka  5778 ka  [C03]           w/=with.  (2000);  [W93],  (1988);



               Zircon U--Th  disequilibrium  age  model  (TIMS)  peak  90 ka o27–ca.  [C05]  54 ka  at  o27–ca. 180 ka peaks  95 ka  and  27  at  [C05]  peaks 200 ka,  45–ca.  104 ka  and  61  at  [C05]  U–Th–Pb).  Charlier  [C00],  al.  et  Wilson





                                                       at  peaks               (e.g.,  2005);  al.,  [W88],
               Zircon U--Th  disequilibrium  age  model  (SIMS)  [C05] 40–52 ka  [C05] 47–69 ka  [C05] 63–76 ka  (+34/ 26) ka–  70  W350 ka  [C03] 60–90 ka  to 50724 ka  W350 ka,  90 ka,  to  70  mean=83714 ka  [C03]  Note: If both 40 Ar/ 39 Ar and K–Ar ages are available only the former are given. 14 C a age determinations are calendar calibrated; Vol  clocks radioacti
                                             [C03]





              40 Ar/ 39 Ar,  K--Ar or  14 C a  age  (eruption)  [N03]  27.3 ka  [N03]  29 ka  45 ka  ca.  [CJNW]  ca.62 ka  inferred  [C03]  [C03]  6272 ka  320–340 ka  [H95]  1.2170.04 Ma  [H95]  other  of  (cited  Wilson  Newnham



                                                      120.5     [H95]  [H95]   those  and  C.J.N.  [N03],
               (km 3 )     [F&L90]  [F&L90]  [F&L90]  [C03]  [C03],  [F&L90]   ages  of  data  (1995);
          (Continued )  Vol  zone  0.5  Tip  3  3  10  flat  caldera  and  volcano  100  caldera  300–1000  300–1000  eruption  unpublished  al.  et




          3                 Rubbish  Dome  caldera?  Earthquake  volcano  xenoliths  Whakamaru  group  ignimbrites  caldera  the  Houghton
          Table  T aupo  volcanic  Poihipi/  Okaia  Tihoi  Another  Okataina  Kapenga  Rotoiti  Rotoiti  Whakamaru  Mangakino  Ongatiti  between  [CJNW],  [H95],
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