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Discovering	
  the	
  NEXT	
  Broken	
  Hill	
  
Mark	
  Dugmore	
  
Broken	
  Hill	
  Symposium	
  27	
  May	
  2015	
  
The	
  in-­‐ground	
  value	
  of	
  the	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  
(pre-­‐mined,	
  pre-­‐eroded)	
  Broken	
  Hill	
  
deposit	
  at	
  current	
  metal	
  prices	
  is	
  
AUD$165	
  Billion	
  
Deposit	
  of	
  NaLonal	
  Interest	
  -­‐	
  Town	
  of	
  NaLonal	
  
Heritage	
  
Assumes:	
  300Mt	
  @	
  148	
  g/t	
  Ag,	
  18.5%	
  combined	
  Pb+Zn.	
  
Source:	
  O’Brien	
  et	
  al,	
  2015	
  
§  Broken	
  Hill	
  is	
  among	
  the	
  great	
  ore	
  deposits	
  of	
  the	
  world	
  
§  Cannington	
  is	
  the	
  world’s	
  largest	
  primary	
  producer	
  of	
  
silver	
  ~30	
  Moz	
  annually	
  
Broken	
  Hill-­‐type	
  Deposits.	
  A	
  big	
  prize!	
  
Mt	
   Ag	
  
g/t	
  
Zn	
  %	
   Pb	
  
%	
  
Ag	
  
Moz	
  
Zn	
  
mt	
  
Pb	
  
mt	
  
Broken	
  Hill	
   300	
   148	
   8.5	
   10.0	
   1,430	
   26	
   30	
  
Cannington	
   44	
   538	
   4.4	
   11.6	
   760	
   2	
   6	
  
Only	
  Five	
  ‘Large’	
  BHT	
  Mines	
  around	
  the	
  World	
  
Large	
  ‘single’	
  deposits	
  dominaLng	
  a	
  district	
  are	
  the	
  norm.	
  
Lower	
  discovery	
  risk	
  exists	
  in	
  NEW	
  districts.	
  
	
  
SchemaLc	
  Broken	
  Hill	
  Type	
  	
  Environment	
  
Host	
  quartzofeldspathic	
  
gneisses,	
  minor	
  amphibolite	
  
*Fe-­‐Mn-­‐Ca-­‐rich	
  ‘iron	
  fm’	
  
Silica	
  ±	
  garnet,	
  
sillimanite,	
  	
  
K-­‐feldspar	
  
Si	
  altera>on,	
  
thin	
  exhalites	
  ±	
  
garnet,	
  gahnite	
  
Bif	
  photo	
  courtesy	
  Steve	
  Walters	
  
K/Na	
  >	
  10.	
  Whole	
  rock	
  Pb	
  to	
  300ppm	
  
500m	
  
How	
  do	
  you	
  airact	
  a	
  BHT!	
  
Follow	
  the	
  Eastern	
  Cratons	
  Margin	
  
§  BHT	
  deposits	
  occur	
  
on	
  the	
  E	
  edge	
  of	
  the	
  
Precambrian	
  
§  IdenLficaLon	
  of	
  a	
  
NEW	
  terrane	
  is	
  
essenLal	
  for	
  a	
  new	
  
discovery	
  
§  Woodmurra	
  is	
  a	
  
NEW	
  terrane	
  	
  
Woodmurra
MagneLcs	
  show	
  the	
  Craton	
  Margin	
  
§  Inferred	
  ‘pop-­‐up’	
  block	
  
of	
  Broken	
  Hill	
  Gp	
  
equivalent	
  
§  Leading,	
  E	
  edge	
  of	
  craton	
  
-­‐	
  magneLcally	
  acLve	
  	
  
§  PaleoProt	
  to	
  MesoProt	
  
metamorphic	
  terrane	
  
Woodmurra
Olympic
Dam
Broken Hill
Woodmurra	
  Project	
  -­‐	
  Geology	
  
Outcrop	
  (to	
  Sth	
  of	
  project)	
  
§  Paleoprot	
  volcano-­‐sedimentary	
  package	
  
§  Age	
  ≡	
  Lower	
  Eastern	
  Succession	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  
(???	
  top	
  of	
  Lower	
  Willyama	
  Supergroup)	
  
§  StraLgraphically	
  below	
  BH	
  &	
  Cannington	
  
Drillholes	
  (to	
  SE	
  of	
  project)*	
  
§  MetasomaLsed	
  qfs	
  gneiss/amphibolite	
  
§  Ca-­‐Mn-­‐Fe-­‐P-­‐F	
  rich	
  assemblages	
  	
  
*	
  
Geophysicists	
  ONE	
  (1)	
  –	
  Geochemists	
  NIL	
  (0)	
  
MagneLcs	
  –	
  Broken	
  Hill	
  
•  Lower,	
  magneLc	
  oxidised	
  felsic-­‐
dominant	
  package	
  
•  Upper,	
  reduced	
  metasediment-­‐
dominant	
  package	
  (mag	
  quiet)	
  
•  ProspecLve	
  ‘TransiLon	
  
Sequence’	
  –	
  in	
  between	
  	
  
–  DisLncLve	
  extensive	
  linear	
  
responses	
  -­‐	
  amphibolites	
  
–  Short	
  strike	
  length	
  Mn-­‐P	
  ‘bif’	
  
	
  
Broken	
  Hill	
  Main	
  Lode	
  
Cannington	
  TMI-­‐RTP	
  &	
  Falcon	
  Airborne	
  Gravity	
  
3,000	
  m	
  
Source:	
  Witherly	
  &	
  Mackee,	
  	
  2015	
  
TMI	
   AGG	
  
•  Overall	
  low	
  magneLc	
  host	
  package	
  
•  MagneLc,	
  short	
  strike	
  length	
  
features	
  with	
  indicaLons	
  of	
  
structural	
  complexity	
  
	
   •  Cannington	
  ore	
  directly	
  
associated	
  with	
  
magneLte	
  
	
  
§  Broken	
  Hill	
  &	
  Cannington	
  lie	
  
near	
  flank	
  of	
  a	
  large	
  gravity	
  high	
  
§  Major	
  ‘gravity	
  gradients’	
  evident	
  
§  Woodmurra	
  shows	
  similariLes	
  
Gravity	
  –	
  Flanks	
  of	
  Highs	
  are	
  Very	
  Important	
  
Cannington	
  
Broken	
  Hill	
  
Main	
  Lode	
  
Images at same scales
Woodmurra	
  
Woodmurra	
  Project	
  –magneLcs	
  
•  Lower,	
  magneLc	
  
package	
  ?quartzo-­‐
feldspathic-­‐rich	
  	
  
•  ProspecLve	
  ‘transiLon’	
  
package	
  with	
  short-­‐strike-­‐
length	
  (bif?)	
  and	
  
disLncLve	
  linear	
  
(amphibolite?)	
  features	
  	
  
•  ‘Feature-­‐deficient’	
  
upper,	
  ?metasediment-­‐
dominated	
  package	
  
	
  
Woodmurra	
  Project	
  –	
  gravity	
  
•  Dense	
  host	
  package	
  
•  ConcentraLon	
  of	
  
amphibolites	
  ???	
  
•  SpaLally	
  associated	
  
with	
  max	
  
development	
  of	
  BHT	
  
mineralisaLon	
  and	
  
lode	
  marker	
  
horizons	
  at	
  BH	
  
	
  
§  Integrate	
  geophysical	
  data	
  from	
  SA	
  Gov’t-­‐funded	
  iniLaLves.	
  
§  Regional	
  magneLcs	
  used	
  to	
  define	
  structure,	
  favourable	
  
lithostraLgraphy	
  and	
  possible	
  direct	
  targets.	
  	
  
§  OLD	
  technology	
  (aeromagneLcs)	
  in	
  a	
  NEW	
  terrane	
  will	
  work.	
  
§  Drill	
  a	
  range	
  of	
  short	
  strike	
  length	
  magneLc	
  anomalies.	
  	
  
§  Aim	
  to	
  i/sect	
  Pb-­‐Mn-­‐P-­‐F	
  anomalous	
  ‘bif’	
  proximal	
  to	
  ore.	
  	
  
Woodmurra	
  Project	
  –	
  Strategy	
  under	
  cover	
  
§  IdenLficaLon	
  of	
  NEW	
  terrane	
  essenLal	
  for	
  discovery	
  of	
  a	
  BHT	
  deposit	
  
§  NEW	
  high	
  grade	
  Proterozoic	
  metamorphic	
  terrane	
  ranked	
  highly	
  as	
  interpreted	
  
NW	
  extension	
  of	
  Broken	
  Hill	
  Block	
  on	
  craton	
  margin	
  
§  MagneLc	
  (short	
  strike	
  length	
  &	
  ‘boat-­‐shaped’	
  anomalies)	
  and	
  gravity	
  seung	
  
(large	
  dense)	
  similar	
  to	
  Broken	
  Hill	
  &	
  Cannington	
  
§  Apparent	
  BHT	
  ‘alteraLon’	
  /	
  ‘unusual’	
  lithologies	
  in	
  previous	
  drilling	
  
§  Outcrop	
  age	
  equivalent	
  to	
  sequence	
  below	
  Cannington	
  &	
  BH	
  
§  Successful	
  PACE	
  Discovery	
  Drilling	
  2015	
  grant	
  
Woodmurra	
  Project	
  –	
  Technical	
  Summary	
  
Reliable	
  Team	
  Required	
  
BHT	
  Minerals	
  Pty	
  Ltd	
  was	
  incorporated	
  in	
  2014	
  to	
  specifically	
  explore	
  for	
  giant	
  
Broken	
  Hill-­‐type	
  (BHT)	
  base-­‐metal	
  deposits	
  within	
  Australia. 	
   	
  	
  
	
  
Who	
  Are	
  BHT	
  Minerals?	
  
Dr	
  Douglas	
  Haynes	
  
Formally	
  Chief	
  Geologist	
  WMC,	
  BHP/BHPBilliton.	
  	
  Key	
  member	
  of	
  
discovery	
  teams	
  on	
  Olympic	
  Dam,	
  Ernest	
  Henry,	
  Kamoa. 	
   	
  	
  
	
  Bob	
  Skrzeczynski	
   	
  	
  
Formally	
  ExploraLon	
  Manager	
  BHP	
  Cannington	
  discovery.	
  
	
  
Mark	
  Dugmore 	
   	
  	
  
Formally	
  ExploraLon	
  Manager	
  BHP,	
  Global	
  Base	
  Metals.	
  
	
  
Discovering	
  the	
  NEXT	
  Broken	
  Hill	
  
Mark	
  Dugmore	
  
Mobile:	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  	
  +61	
  (0)407	
  132	
  975	
  
Email:	
  markdugmore@bigpond.com	
  

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2015 Broken Hill Resources Investment Symposium - BHT Minerals - Mark Dugmore

  • 1. Discovering  the  NEXT  Broken  Hill   Mark  Dugmore   Broken  Hill  Symposium  27  May  2015  
  • 2. The  in-­‐ground  value  of  the                                 (pre-­‐mined,  pre-­‐eroded)  Broken  Hill   deposit  at  current  metal  prices  is   AUD$165  Billion   Deposit  of  NaLonal  Interest  -­‐  Town  of  NaLonal   Heritage   Assumes:  300Mt  @  148  g/t  Ag,  18.5%  combined  Pb+Zn.   Source:  O’Brien  et  al,  2015  
  • 3. §  Broken  Hill  is  among  the  great  ore  deposits  of  the  world   §  Cannington  is  the  world’s  largest  primary  producer  of   silver  ~30  Moz  annually   Broken  Hill-­‐type  Deposits.  A  big  prize!   Mt   Ag   g/t   Zn  %   Pb   %   Ag   Moz   Zn   mt   Pb   mt   Broken  Hill   300   148   8.5   10.0   1,430   26   30   Cannington   44   538   4.4   11.6   760   2   6  
  • 4. Only  Five  ‘Large’  BHT  Mines  around  the  World   Large  ‘single’  deposits  dominaLng  a  district  are  the  norm.   Lower  discovery  risk  exists  in  NEW  districts.    
  • 5. SchemaLc  Broken  Hill  Type    Environment   Host  quartzofeldspathic   gneisses,  minor  amphibolite   *Fe-­‐Mn-­‐Ca-­‐rich  ‘iron  fm’   Silica  ±  garnet,   sillimanite,     K-­‐feldspar   Si  altera>on,   thin  exhalites  ±   garnet,  gahnite   Bif  photo  courtesy  Steve  Walters   K/Na  >  10.  Whole  rock  Pb  to  300ppm   500m  
  • 6. How  do  you  airact  a  BHT!  
  • 7. Follow  the  Eastern  Cratons  Margin   §  BHT  deposits  occur   on  the  E  edge  of  the   Precambrian   §  IdenLficaLon  of  a   NEW  terrane  is   essenLal  for  a  new   discovery   §  Woodmurra  is  a   NEW  terrane     Woodmurra
  • 8. MagneLcs  show  the  Craton  Margin   §  Inferred  ‘pop-­‐up’  block   of  Broken  Hill  Gp   equivalent   §  Leading,  E  edge  of  craton   -­‐  magneLcally  acLve     §  PaleoProt  to  MesoProt   metamorphic  terrane   Woodmurra Olympic Dam Broken Hill
  • 9. Woodmurra  Project  -­‐  Geology   Outcrop  (to  Sth  of  project)   §  Paleoprot  volcano-­‐sedimentary  package   §  Age  ≡  Lower  Eastern  Succession                               (???  top  of  Lower  Willyama  Supergroup)   §  StraLgraphically  below  BH  &  Cannington   Drillholes  (to  SE  of  project)*   §  MetasomaLsed  qfs  gneiss/amphibolite   §  Ca-­‐Mn-­‐Fe-­‐P-­‐F  rich  assemblages     *  
  • 10. Geophysicists  ONE  (1)  –  Geochemists  NIL  (0)  
  • 11. MagneLcs  –  Broken  Hill   •  Lower,  magneLc  oxidised  felsic-­‐ dominant  package   •  Upper,  reduced  metasediment-­‐ dominant  package  (mag  quiet)   •  ProspecLve  ‘TransiLon   Sequence’  –  in  between     –  DisLncLve  extensive  linear   responses  -­‐  amphibolites   –  Short  strike  length  Mn-­‐P  ‘bif’     Broken  Hill  Main  Lode  
  • 12. Cannington  TMI-­‐RTP  &  Falcon  Airborne  Gravity   3,000  m   Source:  Witherly  &  Mackee,    2015   TMI   AGG   •  Overall  low  magneLc  host  package   •  MagneLc,  short  strike  length   features  with  indicaLons  of   structural  complexity     •  Cannington  ore  directly   associated  with   magneLte    
  • 13. §  Broken  Hill  &  Cannington  lie   near  flank  of  a  large  gravity  high   §  Major  ‘gravity  gradients’  evident   §  Woodmurra  shows  similariLes   Gravity  –  Flanks  of  Highs  are  Very  Important   Cannington   Broken  Hill   Main  Lode   Images at same scales Woodmurra  
  • 14. Woodmurra  Project  –magneLcs   •  Lower,  magneLc   package  ?quartzo-­‐ feldspathic-­‐rich     •  ProspecLve  ‘transiLon’   package  with  short-­‐strike-­‐ length  (bif?)  and   disLncLve  linear   (amphibolite?)  features     •  ‘Feature-­‐deficient’   upper,  ?metasediment-­‐ dominated  package    
  • 15. Woodmurra  Project  –  gravity   •  Dense  host  package   •  ConcentraLon  of   amphibolites  ???   •  SpaLally  associated   with  max   development  of  BHT   mineralisaLon  and   lode  marker   horizons  at  BH    
  • 16. §  Integrate  geophysical  data  from  SA  Gov’t-­‐funded  iniLaLves.   §  Regional  magneLcs  used  to  define  structure,  favourable   lithostraLgraphy  and  possible  direct  targets.     §  OLD  technology  (aeromagneLcs)  in  a  NEW  terrane  will  work.   §  Drill  a  range  of  short  strike  length  magneLc  anomalies.     §  Aim  to  i/sect  Pb-­‐Mn-­‐P-­‐F  anomalous  ‘bif’  proximal  to  ore.     Woodmurra  Project  –  Strategy  under  cover  
  • 17. §  IdenLficaLon  of  NEW  terrane  essenLal  for  discovery  of  a  BHT  deposit   §  NEW  high  grade  Proterozoic  metamorphic  terrane  ranked  highly  as  interpreted   NW  extension  of  Broken  Hill  Block  on  craton  margin   §  MagneLc  (short  strike  length  &  ‘boat-­‐shaped’  anomalies)  and  gravity  seung   (large  dense)  similar  to  Broken  Hill  &  Cannington   §  Apparent  BHT  ‘alteraLon’  /  ‘unusual’  lithologies  in  previous  drilling   §  Outcrop  age  equivalent  to  sequence  below  Cannington  &  BH   §  Successful  PACE  Discovery  Drilling  2015  grant   Woodmurra  Project  –  Technical  Summary  
  • 19. BHT  Minerals  Pty  Ltd  was  incorporated  in  2014  to  specifically  explore  for  giant   Broken  Hill-­‐type  (BHT)  base-­‐metal  deposits  within  Australia.         Who  Are  BHT  Minerals?   Dr  Douglas  Haynes   Formally  Chief  Geologist  WMC,  BHP/BHPBilliton.    Key  member  of   discovery  teams  on  Olympic  Dam,  Ernest  Henry,  Kamoa.        Bob  Skrzeczynski       Formally  ExploraLon  Manager  BHP  Cannington  discovery.     Mark  Dugmore       Formally  ExploraLon  Manager  BHP,  Global  Base  Metals.    
  • 20. Discovering  the  NEXT  Broken  Hill   Mark  Dugmore   Mobile:                                  +61  (0)407  132  975   Email:  markdugmore@bigpond.com