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Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil Dionisio Uendro Carlos Leonardo Uieda* Yaoguo Li Valéria Cristina Ferreira Barbosa Marco Antonio Braga Glauco Angeli Guilherme Gravina Peres

Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

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Presentation given on behalf of Dionisio Uendro Carlos at the 2012 SEG Annual Meeting in Las Vegas.

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Page 1: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Iron ore interpretation using gravity-gradient inversions

in the Carajás, Brazil

Dionisio Uendro CarlosLeonardo Uieda*

Yaoguo LiValéria Cristina Ferreira Barbosa

Marco Antonio BragaGlauco Angeli

Guilherme Gravina Peres

Page 2: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Carajás survey area

Page 3: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil
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N1 plateau

Page 7: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

N1 plateau

Target: hematite hard (3.6 g/cm3) soft (3.4 g/cm3)

Page 8: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

N1

Survey

System: FTGLine spacing: 150 mHeight: 100 mTotal survey: ~550 km

Page 9: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

The data

Page 10: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

GzzN1 geology

Page 11: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

GzzN1 geology

Page 12: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

3D inversion

Page 13: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

2 methods

Li, Y. (2001), 3-D inversion of gravity gradiometer data, SEG Expanded Abstracts, 20, 1470–1473, doi:10.1190/1.1816383

Uieda, L., and V. C. F. Barbosa (2012), Robust 3D gravity gradient inversion by planting anomalous densities, Geophysics, 77(4), G55–G66, doi:10.1190/geo2011-0388.1

(1) Planting anomalous densities

(2) Smooth inversion

Page 14: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Planting anomalous densities

Page 15: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Observed data

Mesh

Page 16: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Zero density contrast

Page 17: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Seeds (user specified)

Predicted data

Page 18: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Neighbors

Page 19: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

The best

New predicted data

Page 20: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

The best

New predicted data

φ=√∑i=1

N

(g i−d i)2

min of Γ=φ+μθ

and

compactness

Page 21: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

The best

New predicted data

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Fit

Page 31: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Smooth inversion

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Mesh

Page 33: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

min φ( p)=φd+μφ p

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min φ( p)=φd+μφ p

Densities

Page 35: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

min φ( p)=φd+μφ p

Densities Data misfit

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min φ( p)=φd+μφ p

Densities Data misfit

Smoothness + depth weights

Page 37: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

min φ( p)=φd+μφ p

subject a⩽ p⩽b

Densities Data misfit

Smoothness + depth weights

Page 38: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

True model

Recovered

Page 39: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Different methods

• Different approaches

• Different constraints

• Common data

• Common target

Page 40: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Inversion parameters

• Gzz component = 9,053 obs

• Cell size = 75 m

– Planting = 581,440 cells

– Smooth = 1,520,960 cells (larger mesh)

Page 41: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Seeds

45 seeds

Page 42: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Results

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Smooth

Planting

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Smooth

Planting

Page 47: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Cross-section

Page 48: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Smooth

Page 49: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Smooth

Hematite

Page 50: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Smooth

HematiteJaspilite

Page 51: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Planting anomalous densities

Page 52: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Conclusions

• Joint interpretation

• Preliminary results

• Compatible solutions

• Agree with boreholes

• Concentrated above 300 m

• Bellow 200 m could be jaspilite

– Same density contrast

Page 53: Iron ore interpretation using gravity-gradient inversions in the Carajás, Brazil

Acknowledgements

Colorado School of Mines, USA

Observatório Nacional, Brazil

Vale S.A.