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

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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

description

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

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

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

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Carajás survey area

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N1 plateau

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N1 plateau

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

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N1

Survey

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

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The data

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GzzN1 geology

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GzzN1 geology

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3D inversion

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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

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Planting anomalous densities

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Observed data

Mesh

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Zero density contrast

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Seeds (user specified)

Predicted data

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Neighbors

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The best

New predicted data

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The best

New predicted data

φ=√∑i=1

N

(g i−d i)2

min of Γ=φ+μθ

and

compactness

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The best

New predicted data

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Fit

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Smooth inversion

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Mesh

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min φ( p)=φd+μφ p

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min φ( p)=φd+μφ p

Densities

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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

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min φ( p)=φd+μφ p

subject a⩽ p⩽b

Densities Data misfit

Smoothness + depth weights

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True model

Recovered

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Different methods

• Different approaches

• Different constraints

• Common data

• Common target

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Inversion parameters

• Gzz component = 9,053 obs

• Cell size = 75 m

– Planting = 581,440 cells

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

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Seeds

45 seeds

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Results

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Smooth

Planting

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Smooth

Planting

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Cross-section

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Smooth

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Smooth

Hematite

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Smooth

HematiteJaspilite

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Planting anomalous densities

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Conclusions

• Joint interpretation

• Preliminary results

• Compatible solutions

• Agree with boreholes

• Concentrated above 300 m

• Bellow 200 m could be jaspilite

– Same density contrast

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Acknowledgements

Colorado School of Mines, USA

Observatório Nacional, Brazil

Vale S.A.