3D Prestack Depth Imaging of the Iron-Oxide Deposit in the Ludvika Mining Area (Central Sweden)

Author(s):  
F. Hlousek ◽  
M. Malinowski ◽  
L. Bräunig ◽  
R. Kramer ◽  
S. Buske ◽  
...  
2019 ◽  
Vol 68 (1) ◽  
pp. 24-43 ◽  
Author(s):  
Lena Bräunig ◽  
Stefan Buske ◽  
Alireza Malehmir ◽  
Emma Bäckström ◽  
Monica Schön ◽  
...  

2019 ◽  
Vol 68 (1) ◽  
pp. 7-23 ◽  
Author(s):  
Magdalena Markovic ◽  
Georgiana Maries ◽  
Alireza Malehmir ◽  
Julius Ketelhodt ◽  
Emma Bäckström ◽  
...  

2009 ◽  
Vol 51 (6) ◽  
pp. 520-541 ◽  
Author(s):  
Tong Hou ◽  
Zhaochong Zhang ◽  
Yangsong Du ◽  
Shunting Li

2021 ◽  
Author(s):  
Felix Hloušek ◽  
Michal Malinowski ◽  
Lena Bräunig ◽  
Stefan Buske ◽  
Alireza Malehmir ◽  
...  

Abstract. We present the pre-stack depth imaging results for a case study of 3D reflection seismic exploration at the Blötberget iron-oxide mining site belonging to the Bergslagen mineral district in central Sweden. The goal of this case study is to directly image the ore-bearing units and to map its possible extension down to greater depths than known from existing boreholes. Therefore, we applied a tailored pre-processing workflow as well as two different seismic imaging approaches, Kirchhoff pre-stack depth migration and Fresnel Volume Migration (FVM). Both imaging techniques deliver a well resolved 3D image of the deposit and its host rock, where the FVM image yields a significantly better image quality compared to the KPSDM image. We were able to unravel distinct reflection horizons, which are linked to known mineralisation and provide insights on lateral and depth extent of the deposits beyond their known extension from borehole data. A comparison of the known mineralization and the image show a good agreement of the position and the shape of the imaged reflectors caused by the mineralization. Furthermore, the images show a reflector, which is interpreted to be a fault intersecting the mineralisation and which can be linked to the surface geology. The depth imaging results can serve as the basis for further investigations, drillings and follow-up mine planning at the Blötberget mining site.


Author(s):  
I. L. Cope ◽  
J. J. Wilkinson ◽  
A. J. Boyce ◽  
J. B. Chapman ◽  
R. J. Herrington ◽  
...  

2015 ◽  
Vol 199 ◽  
pp. 95-101 ◽  
Author(s):  
Chuanping Liu ◽  
Huan-Yun Yu ◽  
Chengshuai Liu ◽  
Fangbai Li ◽  
Xianghua Xu ◽  
...  

Solid Earth ◽  
2021 ◽  
Vol 12 (8) ◽  
pp. 1707-1718
Author(s):  
Yinshuai Ding ◽  
Alireza Malehmir

Abstract. To discover or delineate mineral deposits and other geological features such as faults and lithological boundaries in their host rocks, seismic methods are preferred for imaging the targets at great depth. One major goal for seismic methods is to produce a reliable image of the reflectors underground given the typical discontinuous geology in crystalline environments with low signal-to-noise ratios. In this study, we investigate the usefulness of the reverse time migration (RTM) imaging algorithm in hardrock environments by applying it to a 2D dataset, which was acquired in the Ludvika mining area of central Sweden. We provide a how-to solution for applications of RTM in future and similar datasets. When using the RTM imaging technique properly, it is possible to obtain high-fidelity seismic images of the subsurface. Due to good amplitude preservation in the RTM image, the imaged reflectors provide indications to infer their geological origin. In order to obtain a reliable RTM image, we performed a detailed data pre-processing flow to deal with random noise, near-surface effects, and irregular receiver and source spacing, which can downgrade the final image if ignored. Exemplified with the Ludvika data, the resultant RTM image not only delineates the iron oxide deposits down to 1200 m depth as shown from previous studies, but also provides a better inferred ending of sheet-like mineralization. Additionally, the RTM image provides much-improved reflection of the dike and crosscutting features relative to the mineralized sheets when compared to the images produced by Kirchhoff migration in the previous studies. Two of the imaged crosscutting features are considered to be crucial when interpreting large-scale geological structures at the site and the likely disappearance of mineralization at depth. Using a field dataset acquired in hardrock environment, we demonstrate the usefulness of RTM imaging workflows for deep targeting mineral deposits.


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