Seismic interferometry for mineral exploration

Passive seismic experiment over kylylahti mine area, Finland

Conference Paper (2018)
Author(s)

M. Chamarczuk (Polish Academy of Sciences)

M. Malinowski (Polish Academy of Sciences)

D. Draganov (TU Delft - Civil Engineering & Geosciences)

E. Koivisto (University of Helsinki)

S. Heinonen (Geological Survey of Finland)

S. Juurela (Boliden FinnEx)

Contributor(s)

Research Group
Applied Geophysics and Petrophysics
DOI related publication
https://doi.org/10.3997/2214-4609.201802703 Final published version
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Publication Year
2018
Language
English
Research Group
Applied Geophysics and Petrophysics
Article number
Tu 2MIN 03
ISBN (electronic)
9789462822658
Event
2nd Conference on Geophysics for Mineral Exploration and Mining (2018-09-09 - 2018-09-13), Porto, Portugal
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Abstract

We present the results of adapting seismic interferometry (SI) for reflection imaging in mineral exploration. We use a unique dataset of one-month ambient-noise recordings acquired with large-N array (~1000 receivers) deployed in a regular grid (50 m receiver interval, 200 m line interval) directly above the known mineralisation and underground mine infrastructure at the Kylylahti polymetallic mine located in Eastern Finland. Ambient-noise in the study area is dominated by the road traffic and mine activities (both surface and underground) providing quasi omni-directional distribution and broad freqeuncy spectrum of the noise sources. We start from the simple 2D forward modelling using existing geological model. Results of the SI applied to field data from selected receiver lines exhibit reflections related to the bottom of the ore body as well as the reflection from the target area confirmed by synthetics. Finally, we develop robust mineral exploration SI workflow (MESI) tailored for reflection imaging and apply it to our 3D ambient-noise dataset. Migrated sections obtained from the MESI-processed data exhibit high reflectivity, compatible with the active-source seismics and directly related to the known geological structures.

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