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# Lower crustal resistivity signature of an orogenic gold system

## Abstract

Orogenic gold deposits provide a significant source of the world’s gold and form along faults over a wide range of crustal depths spanning sub-greenschist to granulite grade faces, but the source depths of the gold remains poorly understood. In this paper we compiled thirty years of long-period magnetotelluric (MT) and geomagnetic depth sounding (GDS) data across western Victoria and south-eastern South Australia that have sensitivity to the electrical resistivity of the crust and mantle, which in turn depend on past thermal and fluid processes. This region contains one of the world’s foremost and largest Phanerozoic (440 Ma) orogenic gold provinces that has produced 2% of historic worldwide gold production. Three-dimensional inversion of the long-period MT and GDS data shows a remarkable correlation between orogenic gold deposits with > 1 t production and a < 20 Ω m low-resistivity region at crustal depths > 20 km. This low-resistivity region is consistent with seismically-imaged tectonically thickened marine sediments in the Lachlan Orogen that contain organic carbon (C), sulphides such as pyrite (FeS2) and colloidal gold (Au). Additional heat sources at 440 Ma due to slab break-off after subduction have been suggested to rapidly increase the temperature of the marine sediments at mid to lower crustal depth, releasing HS ligands for Au, and CO2. We argue that the low electrical resistivity signature of the lower crust we see today is from a combination of flake graphite produced in situ from the amphibolite grade metamorphism of organic-carbon in the marine sediments, and precipitated graphite through retrograde hydration reactions of CO2 released during the rapid heating of the sediments. Thus, these geophysical data image a fossil source and pathway zone for one of the world’s richest orogenic gold provinces.

## Introduction

Orogenic gold deposits in upper crustal settings are a significant source of the world’s gold resources, but their origin depth is contentious 1,2,3,4,5,6,7,8 The 440 Ma orogenic belt in south eastern Australia is one of the largest global gold provinces and had been widely researched in terms of its structural and geodynamic setting 9,10,11,12 but the 3D crustal architecture is poorly constrained13. To provide new insight on the crustal structure beneath this gold province, we have compiled 30 years of broadband and long-period MT and GDS surveys across western Victoria and south-eastern South Australia 20,21. Since 2013, high-quality long-period MT data have been collected in the Australian Lithospheric Architecture Magnetotelluric Project (AusLAMP) with site spacing of approximately 55 km22,23 that covers all of South Australia and Victoria. After removal of poor-quality sites, 123 long-period MT and GDS sites, 252 broadband MT (mostly with GDS data) and 40 long-period GDS sites were identified as a composite database, covering an area approximately 800 km east–west and 500 km north–south, as shown in Fig. 1.

Three-dimensional inversion of all long-period MT (123 sites) and long-period GDS (40 sites) data, including bathymetry and topography, produced a model that fits the full tensor data to an RMS misfit of 2.1, with error floors of 5% for each impedance element and 0.02 for magnetic transfer functions. A number of different inversions were undertaken, testing: (a) models with and without inversion for distortion; (b) changes in the depth-weighting of smoothness parameters; (c) varying levels of horizontal and vertical regularization; and (d) models with and without near-surface (top 3 km and top 500 m) smoothing. Broadband MT data were not included in the three-dimensional inversion as they have quite a different spatial and frequency sampling14,15,16,17,18,19. However, we use these data to verify the results from the three-dimensional inversion in the Supplementary Information.

Figure 2 shows three depth slices from the preferred model at lower-crustal depths of (a) 20 and (b) 30 km, and (c) at the lithosphere-asthenosphere boundary depth of ~ 150 km. Details of the 3D inversion parameters are provided in the Supplementary Information and Fig. S1. Additional slices at 5, 10, 40, and 100 km are also shown in Supplementary Information, Fig. S2a–d. At 30 km, there is a strong spatial correlation between major orogenic gold deposits around Ballarat and Bendigo and low-resistivity regions < 20 Ωm.

Such low crustal resistivities in silicate minerals are unlikely to be solely due to temperature, even if minerals are significantly hydrated25, so another mechanism to enhance conduction is required26. Such additional conduction is generally argued to be graphite26,27, magnetite and sulphides25,28, or sometimes free fluids29,30, which are secondary overprints of the primary crustal materials31. Of these competing mechanisms, magnetite and sulphides are generally of negligible volume and are isolated in fresh xenolith granulites25, and are unlikely to interconnect over tens of kilometres. Similarly, aqueous fluids are unlikely to be stable and connected over long geological time scales32.Thus, the mostly commonly proposed mechanism for widespread electrical conduction at lower crustal depths is graphite31,27.

Large et al.33 argue that Au deposits in orogenic settings are originally sourced from marine sediments in deep ocean environments that host C, FeS2 and potentially colloidal Au. When buried to mid to lower crust depths, and with additional rapid heating from the upper mantle6,7,9 such oceanic sediments rich in C and FeS2 generate significant amounts of free aqueous sulphur (HS,S2−) in a relatively short time frame that acts as the ligand for Au through the following relationship7.

$${\text{2FeS}}_{{2}} + {\text{ 2H}}_{{2}} {\text{O }} + {\text{ C }} = {\text{ 2FeS }} + {\text{ 2H}}_{{2}} {\text{S }} + {\text{ CO}}_{{2}}$$

For the case of the Victorian gold province the additional heat source at 440 Ma has been suggested to be due to slab break-off and subsequent mantle upwelling that allowed a rapid introduction of mantle heat into the crust10. This mechanism is thought to have occurred along many hundreds of kilometres of a mega-subduction zone off the eastern margin of Gondwana, explaining the widespread occurrences of world-class orogenic and instruction-related gold deposits that were formed simultaneously in the Lachlan Orogen at 440 Ma10.

Organic carbon in sediment may be metamorphosed to flake graphite at amphibolite grade conditions at depths of ~ 20–30 km and temperatures ~ 550 °C34. In addition, mobilised CO2 may be precipitated as graphite35,36 either at grain boundaries27 or along more permeable zones37,38 through retrograde hydration reactions where the host-rock oxygen fugacity (fO2 rock) is below the upper fO2 limit of graphite39. We argue, therefore, that the low resistivity imaged ~ 30 km depth may be due to graphite. At 20 km depth, the zone of lower resistivity is narrowed and major deposits appear to align along the western margin of the resistivity anomaly, suggesting that the pathway of Au deposits to the surface is controlled by variations in permeability that are expressed as gradients in electrical properties. The resistive western flank may represent a permeability boundary that is structurally aligned with the Heathcote Fault Zone24,40. Deposits to the west of the low-resistivity zone at 30 km depth, particularly in the Stawell area, are porphyritic and instruction-related rather than orogenic11,42,44.

Figure 2 shows an additional zone of low resistivity of < 300 Ωm centred around the town of Mount Gambier. It is most evident as a separate region in the 20 km depth slice; at 30 km depth the region has slightly lower resistivity (minimum 100 Ωm), but the inherent smoothing of the three-dimensional modelling with increasing depth merges these features. We argue that the cause of this lower resistivity at crustal depths may be due to hotter temperatures associated with the Newer Volcanic Province43,44,45,46,47,48,49,50. The most recent volancism (~ 4.5 ka) at Mount Schank, 10 km south of Mount Gambier (volcanism 5 ka), indicates that higher crustal temperatures are still present. For the 20 and 30 km depth slices, an order of magnitude decrease in resistivity (1000 to 100 Ωm) can be explained by thermal anomalies of 100 °C25.

At the base of the lithosphere, at a depth of ~ 150 km, there is a resistivity gradient of > 1000 Ωm to 100 Ωm from the southern Delamerian Orogen to the Lachlan Orogen. This trend is also seen in an eastward reduction of P and S-wave velocities13 suggesting that there is a step in lithospheric thickness due to higher temperatures beneath the Lachlan orogenic belts.

Reflection seismic profiles 06GA-V1 to V3 were collected across the western Victorian goldfields in 200612,24, as shown in Fig. 2b. In Fig. 3 we show a cross-section from the resistivity model along the seismic lines 06GA-V1 to V3 with a structural interpretation derived from the seismic data24,40. The resistivity model is a smoothed representation of the geology, but clearly shows that the low-resistivity region (< 20 Ωm) lies near the boundary between the Bendigo Zone and the Selwyn Block in Fig. 3. This low-resistivity region extends from a depth of about 20 km to the seismically defined Moho, and is centred on the west-dipping listric Heathcote Fault Zone, which bounds the Proterozoic Selwyn Block47. The east-dipping Moyston Fault that is recognized as the boundary between the Delamerian and Lachlan Orogens24 has a less pronounced electrical signature, but delineates the western extent of the low-resistivity region in the lower crust.

The most electrically conductive zone in Fig. 3 is in a broad region of shearing where oceanic mafic crustal elements are highly faulted and stacked above and below the Heathcote Fault Zone23,24, representing a zone of enhanced transient permeability during tectonism. The lower resistivity observed along the Heathcote Fault Zone may represent a zone of enhanced graphite deposition from CO2-rich fluids27,37,38 evolved from tectonically thickened carbon-rich sediments.

## Conclusions

We conclude that the south-eastern Australia orogenic gold deposits have a deep crustal origin. Such gold deposits are spatially correlated with a broad region of lower crust (> 20 km depth) with electrical resistivity of less than 20 Ωm. We argue that this footprint of the source is due to the presence of graphite derived from carbon and pyrite-rich source sediments, from direct metamorphism to flake graphite and precipitated graphite through retrograde hydration reactions of CO2 released from the sediments.

## Methods

MT and GDS responses used in the inversion were rotated to 305° (clockwise from geographic N), in line with the 3D mesh orientation. The orientation was primarily chosen to parallel the orientation of the continental shelf and slope to the south. Data were resampled to five per decade over a bandwidth from 10 to 10,000 s, for a total of 16 periods. Error floors of 5% for all tensor impedances and 0.02 for magnetic transfer functions were assigned. Static distortion matrices were also determined from the inversion.

Cell width in the core area is 5 km and the core extended beyond sites by 30 km (6 cells). Lateral padding of 500 km was included, with a growth factor of 1.3. Vertical spacing starts from 100 m at the topographic level, increasing by a factor of 1.06 per cell down to 10 km depth, 1.04 per cell to 100 km, and finally 1.2 until the bottom of the mesh at 800 km. The model includes bathymetry and topography: starting resistivity is a homogenous 200 Ωm, and 0.25 Ωm for sea water. The final model comprised 189 by 123 cells, and 115 layers, to give a total of 2,673,405 free parameters.

## Data availability

All MT and GDS data are available from the Geoscience Australia (https://doi.org/10.11636/Record.2018.021), the State Government of South Australia (map.sarig.sa.gov.au/) and National Computational Infrastructure (www.nci.org.au/).

## References

1. Groves, D. I. & Santosh, M. Province-scale commonalities of some world-class gold deposits: Implications for mineral exploration. Geosci. Front. 6, 389–399. https://doi.org/10.1016/j.gsf.2014.12.007 (2015).

2. Goldfarb, R. J. & Groves, D. I. Orogenic gold: Common or evolving fluid and metal sources through time. Lithos 233, 2–26. https://doi.org/10.1016/j.lithos.2015.07.011 (2015).

3. Tomkins, A. G. A biogeochemical influence on the secular distribution of orogenic gold. Econ. Geol. 108, 193–197. https://doi.org/10.2113/econgeo.108.2.193 (2013).

4. Groves, D. I. & Bierlein, F. P. Geodynamic settings of mineral deposit systems. J. Geol. Soc. 164, 19–30. https://doi.org/10.1144/0016-76492006-065 (2007).

5. Groves, D. I., Goldfarb, R. J. & Santosh, M. The conjunction of factors that lead to formation of giant gold provinces and deposits in non-arc settings. Geosci. Front. 7, 303–314. https://doi.org/10.1016/j.gsf.2015.07.001 (2016).

6. Gaboury, D. Does gold in orogenic deposits come from pyrite in deeply buried carbon-rich sediments?: Insight from volatiles in fluid inclusions. Geology 41, 1207–1210. https://doi.org/10.1130/G34788.1 (2013).

7. Gaboury, D. Parameters for the formation of orogenic gold deposits. Appl. Earth Sci. 128, 124–133. https://doi.org/10.1080/25726838.2019.1583310 (2019).

8. Groves, D. I., Santosh, M. & Zhang, L. A scale-integrated exploration model for orogenic gold deposits based on a mineral system approach. Geosci. Front. 11, 719–738. https://doi.org/10.1016/j.gsf.2019.12.007 (2020).

9. Phillips, D. et al. Timing of gold mineralisation in the western Lachlan orogen, SE Australia: A critical overview. Aust. J. Earth Sci. 59, 495–525. https://doi.org/10.1080/08120099.2012.682738 (2012).

10. Vos, I. M. A., Bierlein, F. P. & Heithersay, P. S. A crucial role for slab break-off in the generation of major mineral deposits: insights from central and eastern Australia. Miner. Deposita 42, 515–522. https://doi.org/10.1007/s00126-007-0137-3 (2007).

11. Vos, I. M. A., Bierlein, F. P., Heithersay, P. S., & Lister, G. S. Geodynamic controls on giant metallogenic provinces: Insights from gold provinces in southeast Australia. In: (eds. Mao, J, & Bierlein, F.P.) Mineral deposit research: Meeting the global challenge. https://doi.org/10.1007/3-540-27946-6_16 (Springer, Berlin, 2005).

12. Willman, C. E. et al. Crustal-scale fluid pathways and source rocks in the Victorian gold province, Australia: Insights from deep seismic reflection profiles. Econ. Geol. 105, 895–915. https://doi.org/10.2113/gsecongeo.105.5.895 (2010).

13. Rawlinson, N., Pilia, S., Young, M., Salmon, M. & Yang, Y. Crust and upper mantle structure beneath southeast Australia from ambient noise and teleseismic tomography. Tectonophysics 689, 143–156. https://doi.org/10.1016/j.tecto.2015.11.034 (2016).

14. Dennis, Z. R., Moore, D. H. & Cull, J. P. A geological interpretation of the Echuca magnetotelluric survey, Victoria. Aust. J. Earth Sci. 58, 587–597. https://doi.org/10.1080/08120099.2011.577808 (2011).

15. Dennis, Z. R., Moore, D. H. & Cull, J. P. Magnetotelluric survey for undercover structural mapping, Central Victoria. Aust. J. Earth Sci. 58, 33–47. https://doi.org/10.1080/08120099.2011.534817 (2011).

16. Dennis, Z. R., Thiel, S. & Cull, J. P. Lower crust and upper mantle electrical anisotropy in southeastern Australia. Explor. Geophys. 43, 228–241. https://doi.org/10.1071/EG11022 (2012).

17. Aivazpourporgou, S., Thiel, S., Hayman, P. C., Moresi, L. N. & Heinson, G. Decompression melting driving intraplate volcanism in Australia: Evidence from magnetotelluric sounding. Geophys. Res. Lett. 42, 346–354. https://doi.org/10.1002/2014GL060088 (2015).

18. Robertson, K. E., Heinson, G. S., Taylor, D. H. & Thiel, S. The lithospheric transition between the Delamerian and Lachlan orogens in western Victoria: New insights from 3D magnetotelluric imaging. Aust. J. Earth Sci. 64, 385–399. https://doi.org/10.1080/08120099.2017.1292953 (2017).

19. Robertson, K., Taylor, D., Thiel, S. & Heinson, G. Magnetotelluric evidence for serpentinisation in a Cambrian subduction zone beneath the Delamerian Orogen, southeast Australia. Gondwana Res. 28, 601–611. https://doi.org/10.1016/j.gr.2014.07.013 (2015).

20. Whellams, J. M. Spatial inhomogeneity of geomagnetic fluctuation fields and their influence on high resolution aeromagnetic surveys. PhD Thesis, Flinders University, South Australia (1996).

21. Milligan, P. R., White, A., Heinson, G. & Brodie, R. Micropulsation and induction array study near Ballarat victoria. Explor. Geophys. 24, 117–122. https://doi.org/10.1071/EG993117 (1993).

22. Robertson, K., Heinson, G. & Thiel, S. Lithospheric reworking at the proterozoic-phanerozoic transition of Australia imaged using AusLAMP magnetotelluric data. Earth Planet. Sci. Lett. 452, 27–35. https://doi.org/10.1016/j.epsl.2016.07.036 (2016).

23. Kirkby, A. L. et al. Lithospheric architecture of a Phanerozoic orogen from magnetotellurics: AusLAMP in the Tasmanides, southeast Australia. Tectonophysics 793, 228560. https://doi.org/10.1016/j.tecto.2020.228560 (2020).

24. Cayley, R. A. et al. Crustal architecture of central Victoria: Results from the 2006 deep crustal reflection seismic survey. Aust. J. Earth Sci. 58, 113–156. https://doi.org/10.1080/08120099.2011.543151 (2011).

25. Yang, X. Origin of high electrical conductivity in the lower continental crust: A review. Surv. Geophys. 32, 875–903. https://doi.org/10.1007/s10712-011-9145-z (2011).

26. Glover, P. W. J. Graphite and electrical conductivity in the lower continental crust: A review. Phys. Chem. Earth 21, 279–287 (1997).

27. Frost, B. R., Fyfe, W. S., Tazaki, K. & Chan, T. Grain-boundary graphite in rocks and implications for high electrical conductivity in the lower crust. Nature 340, 134–136. https://doi.org/10.1038/340134a0 (1989).

28. Reynard, B., Mibe, K. & Moortèle, B. D. Electrical conductivity of the serpentinised mantle and fluid flow in subduction zones. Earth Planet. Sci. Lett. 307, 387–394 (2011).

29. Hyndman, R. D., Vanyan, L. L., Marquis, G. & Law, L. K. The origin of electrically conductive lower continental crust: Saline water or graphite?. Phys. Earth Planet. Int. 81, 325–344 (1993).

30. Simpson, F. Fluid trapping at the brittle-ductile transition re-examined. Geofluids 1, 123–136. https://doi.org/10.1046/j.1468-8123.2001.00011.x (2001).

31. Selway, K. On the causes of electrical conductivity anomalies in tectonically stable lithosphere. Surv. Geophys. 35, 219–257. https://doi.org/10.1007/s10712-013-9235-1 (2014).

32. Yardley, B. W. D. & Valley, J. W. The petrologic case for a dry lower crust. J. Geophys. Res. Solid Earth 102, 12173–12185. https://doi.org/10.1029/97JB00508 (1997).

33. Large, R. R., Bull, S. W. & Maslennikov, V. V. A carbonaceous sedimentary source-rock model for carlin-type and orogenic gold deposits. Econ. Geol. 106, 331–358. https://doi.org/10.2113/econgeo.106.3.331 (2011).

34. Rosing-Schow, N. et al. Hydrothermal flake graphite mineralisation in Paleoproterozoic rocks of south-east Greenland. Miner. Deposit. 52, 769–789. https://doi.org/10.1007/s00126-016-0701-9 (2017).

35. Buseck, P. R. & Beyssac, O. From organic matter to graphite: Graphitization. Elements 10, 421–426. https://doi.org/10.2113/gselements.10.6.421 (2014).

36. Rumble, D. Hydrothermal graphitic carbon. Elements 10, 427–433. https://doi.org/10.2113/gselements.10.6.427 (2014).

37. Jodicke, H., Nover, G., Kruhl, J. H. & Markfort, R. Electrical properties of a graphite-rich quartzite from a former lower continental crust exposed in the Serre San Bruno, Calabria (southern Italy). Phys. Earth Planet. Int. 165, 56–67. https://doi.org/10.1016/j.pepi.2007.08.001 (2007).

38. MonteiroSantos, F. A., Mateus, A., Almeida, E. P., Pous, J. & Mendes-Victor, L. A. Are some of the deep crustal conductive features found in SW Iberia caused by graphite?. Earth Planet. Sci. Lett. 201, 353–367. https://doi.org/10.1016/S0012-821X(02)00721-5 (2002).

39. Huizenga, J. M. & Touret, J. L. R. Granulites, CO2 and graphite. Gondwana Res. 22, 799–809. https://doi.org/10.1016/j.gr.2012.03.007 (2012).

40. Wilson, C. J. L. & Leader, L. D. Modeling 3D crustal structure in Lachlan Orogen, Victoria, Australia: Implications for gold deposition. J. Struct. Geol. 67, 235–252. https://doi.org/10.1016/j.jsg.2014.01.007 (2014).

41. Squire, R. & Miller, J. Synchronous compression and extension in East Gondwana: Tectonic controls on world-class gold deposits at 440 Ma. Geology 31, 1073. https://doi.org/10.1130/G19710.1 (2003).

42. Hronsky, J. M. A., Groves, D. I., Loucks, R. R. & Begg, G. C. A unified model for gold mineralisation in accretionary orogens and implications for regional-scale exploration targeting methods. Miner. Deposit. 47, 339–358. https://doi.org/10.1007/s00126-012-0402-y (2012).

43. Boyce, J. The Newer Volcanics Province of southeastern Australia: A new classification scheme and distribution map for eruption centres. Aust. J. Earth Sci. 60, 449–462. https://doi.org/10.1080/08120099.2013.806954 (2013).

44. Boyce, J., Nicholls, I., Keays, R. & Hayman, P. Victoria erupts: The Newer Volcanics Province of south-eastern Australia. Geol. Today 30, 105–109. https://doi.org/10.1111/gto.12054 (2014).

45. Cas, R. A. F., van Otterloo, J., Blaikie, T. N. & van den Hove, J. in Geological Society Special Publication Vol. 446, 123–172 (2017).

46. Mather, B., McLaren, S., Taylor, D., Roy, S., Moresi, L. Variations and controls on crustal thermal regimes in Southeastern Australia. Tectonophysics 723261–276 https://doi.org/10.1016/j.tecto.2017.12.015 (2018)

47. Cayley, R. A., Taylor, D. H., VandenBerg, A. H. M. & Moore, D. H. Proterozoic: Early palaeozoic rocks and the tyennan orogeny in central Victoria: The Selwyn Block and its tectonic implications. Aust. J. Earth Sci. 49, 225–254. https://doi.org/10.1046/j.1440-0952.2002.00921.x (2002).

48. LaRowe, D. E. et al. The fate of organic carbon in marine sediments: New insights from recent data and analysis. Earth Sci. Rev. 204, 103146. https://doi.org/10.1016/j.earscirev.2020.103146 (2020).

49. Wilkin, R. T. in Encyclopedia of Sediments and Sedimentary Rocks (eds Gerard V. Middleton et al.) 701–703 (Springer, 2003).

50. Glassley, W. Fluid evolution and graphite genesis in the deep continental crust. Nature 295, 229–231 (1982).

## Acknowledgements

The AusLAMP projects in SA and Victoria provided the core data sets for the three-dimensional modelling. Additional long-period MT and GDS data were provided by S Aivazpourporgou and J Whellams. Broadband MT data sets were made available by Z Dennis, the University of Adelaide and the Geological Survey of Victoria. The AusLAMP Victoria data were collected under a collaborative project between the Geological Survey of Victoria and Geoscience Australia using Australian Government NCRIS Capability AuScope and Geoscience Australia instruments. The AusLAMP South Australia data were collected using AuScope instruments by the Geological Survey of South Australia, the University of Adelaide and Geoscience Australia, with acquisition funded from the Geological Survey of South Australia, Geoscience Australia and AuScope. The authors acknowledge the many people from Geoscience Australia, Geological Survey of South Australia, Geological Survey of Victoria and the University of Adelaide involved in collecting the data and the support provided by individuals and communities to access the country, especially in remote and rural Australia. The authors acknowledge the traditional custodians of the land on which the data in this paper were collected. Alison Kirkby and Jingming Duan publish with the permission of the CEO, Geoscience Australia. Stephan Thiel and Kate Robertson publish with the permission of the CEO, Geological Survey of South Australia. We thank Dr Chris Lawley and an anonymous reviewer for the constructive comments that have significantly improved the manuscript.

## Author information

Authors

### Contributions

G.H. compiled the data sets, and wrote the paper with input from all other authors. J.D. and A.K. provided the AusLAMP Victoria data, S.T. and K.R. provided the AusLAMP SA data, and S.A. provided a smaller grid of long period MT collected in Western Victoria. W.S. undertook the three-dimensional numerical modelling.

### Corresponding author

Correspondence to Graham Heinson.

## Ethics declarations

### Competing interests

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Heinson, G., Duan, J., Kirkby, A. et al. Lower crustal resistivity signature of an orogenic gold system. Sci Rep 11, 15807 (2021). https://doi.org/10.1038/s41598-021-94531-8

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• DOI: https://doi.org/10.1038/s41598-021-94531-8

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