Abstract
Chile is a very important country that forms part of the Andean metallogenic belts. The Atacama and Domeyko fault systems in northern Chile control the tectonic–magmatic activities that migrate eastward and the types of mineral resources. In this paper, we processed and interpreted aeromagnetic data from northern Chile using reduction to pole, upward field continuation, the second derivative calculation in the vertical direction, inclination angle calculation, and analytical signal amplitude analysis. We revealed the locations and planar distribution characteristics of the regional deep faults along the NNE and NS directions. Furthermore, we observed that the major reasons for the formation of the tectonic–magmatic rocks belts were the nearly parallel deep faults distributed from west to east and multiple magmatic activities along these faults. We ascertained the locations of volcanic mechanisms and the relationships between them using these regional deep faults. We deduced the spatial distributions of the basic–intermediate, basic, and acidic igneous rocks, intrusive rocks, and sedimentary sequences. We showed the linear positive magnetic anomalies and magnetic anomaly gradient zones by slowly varying the background, negative magnetic anomaly field, which indicated the presence of strong magmatic activities in these regional deep faults; it also revealed the favorable areas of copper and polymetallic mineralization. This study provides some basic information for further research on the geology, structural characteristics, and mineral resource prospecting in northern Chile.
Similar content being viewed by others
References
Al Kadasi, A. N., 2015, Interpretation of aeromagnetic data in terms of surface and subsurface geologic structures, southwestern Yemen: Arab J. Geosci., 8, 1163–1179.
Armijo, R., and Thiele, R., 1990, Active faulting in northern Chile: ramp stacking and lateral decoupling along a subduction plate boundary?: Earth and Planetary Science Letters, 98, 40–61.
Brown, M., Diáz, F., and Grocott, J., 1993, Displacement history of the Atacama fault system 25°S–27°S, northern Chile: Geological Society of America Bulletin, 105, 1165–1174.
Camus, F., and Dilles, J. H., 2001, Special issue devoted to porphyry copper deposits of northern Chile: Preface. Economic Geology, 96, 233–237.
Chorowicz, J., Vicente, J. C., Chotin, P., and Mering, C., 1996, Neotectonic map of the Atacama Fault Zone (Chile) from SARS ERS-1 images: Third ISAG, 165–168.
Elderry, S. M., Diaz, G. C., Prior, D. J., and Flint, S. S., 1996, Structural styles in the Domeyko range, northern Chile: Third ISAG, St Malo (France), 9, 17–19.
Eppelbaum, L. V., 2015, Quantitative interpretation of magnetic anomalies from bodies approximated by thick bed models in complex environments: Environ Earth Sci., 74, 5971–5988.
Fang, W. X., and Li, J. X., 2014, Metallogenic regulations, controlling factors, and evolutions of iron oxide copper and gold deposits in Chile: Advances in Earth Science, 29(9), 1011–1024. (in Chinese with English abstract).
Fu, C. C., 2013, Geological characteristics, metallogenic mechanism and prospecting direction of the MANUEL copper deposit: Journal of East China Institute of Technology, 36(s1), 15–19 (in Chinese with English abstract).
He, M. S., Tang, K., and Zou, G. S., 2014, Geological characteristics and metallogenic regularity of the porphyry copper deposits in Chile: Geology and Resources, 23(3), 305–310 (in Chinese with English abstract).
Hinze, W. J., and Von Frese, R. R. B., 1990, Magnetics in geoexploration: Proc. India Acad. Sci. (Earth Planet Sci.), 99(4), 515–547.
Huang, L. P., and Guan, Z. N., 1998, The determination of magnetic causative boundaries using total gradient modules of magnetics anomalies: Journal of East China Geological Institute, 21(2), 143–150 (in Chinese with English abstract).
Jensen, E., Cembrano, J., Faulkner, D., Veloso, E., and Arancibia, G., 1996, Development of a self-similar strike-slip duplex system in the Atacama Fault system, Chile: Journal of Structural Geology, 33(11), 1611–1626.
Li, J. X., and Fang, W. X., 2011, Control of structure and magma for Iron Oxide copper gold and porphyry Copper gold deposits: China Mining Magazine, 20(10), 57–61 (in Chinese with English abstract).
Li, J. X., Fang, W. X., and Liu, J. J., 2009, The strikeslip expansion and ore controlling of the Atacama fault zone in Chile: Journal of Mineral, (suppl), 180–181 (in Chinese with English abstract).
Li, J. X., Fang, W. X., and Liu, J. J., 2011a, Types and characteristics of regional tectonic and ore-field structures of iron oxide-copper-gold deposits in Chile: Geology and Exploration, 47(2), 323–332 (in Chinese with English abstract).
Li, J. X., Zhang, H. Y., and Gao, H. O., 2011b, Geological characteristics and ore marks for prospecting of Los Quilos copper deposit in Chile: Contribution to Geology and Mineral Resources Research, 26(1), 85-59 (in Chinese with English abstract).
Li, T. C., Yang, X. Y., Peng, X. M., Hu, L. G., Wang, L., and Chen, J. L., 2015, Geological characteristics and prospecting criteria of the magnetite deposits in Cerro Iman-Cerro Lunar-Cerro Norte area, central-northern Chile: Mineral Exploration, 6(1), 77–85 (in Chinese with English abstract).
Liu, Y. X., 2007, Evaluation and extraction of weak gravity and magnetic anomalies: Applied Geophysics, 4(4), 288–293.
Liu, Y. X., He, Z. X., Zhang, B. T., Dong, W. B., and Li, D. C., 2006, Integrated geophysical technique for identification of igneous rocks: Progress in Exploration Geophysics, 29(2), 115–118 (in Chinese with English abstract).
Lu, J., Fang, W. X., and Li, T. C., 2013, Analysis on relationships between Magnetic susceptibility and density of rock and ore in the Moon mountain iron copper deposit in Chile: Metal Mine, 445, 105–108 (in Chinese with English abstract).
Lucassen, F., Becchio R., Harmon, R., Kasemann, S., Franz, G., Trumbull, R., Wilke H. G., Romer, R. L., and Dulski, P., 2001, Composition and density model of the continental crust at an active continental margin-the Central Andes between 21S and 27S: Tectonophysics, 341, 195–223.
Mei, Y. X., Pei, R. F., Yang, D. F., Da, Z. X., Li, J. W., Xu, C. R., and Qu, H. Y., 2009, Global metallogenic domains and districts: Mineral Deposits, 28(4), 383–389 (in Chinese with English abstract).
Miller, H. G., and Singh, V., 1994, Potential field tilt-A new concept for location of potential field source: Journal of Applied Geophysics, 32(2), 213–217.
Niemeyer, H., and Urrutia, C., 2009, Strike-slip along the Sierra de Varas Fault (Cordillera de Domeyko Fault-System), northern Chile: Andean Geology, 36(1), 37–49 (in Spanish).
Ranganai, R. T., Whaler, A. A., and Ebinger, C. J., 2015, Aeromagnetic interpretation in the south-central Zimbabwe Craton: (reappraisal of) crustal structure and tectonic implications: International Journal of Earth Sciences (GeolRundsch), 1–27.
Ren, A. J., Jin, Q. M., Jing, F. J., and Liang, Y., 1993, Mesozoic tectonic evolution of southern Andes: Volcanology and Mineral Resources, 14(4), 126 (in Chinese with English abstract).
Richards, J. P., Boyce, A. J., and Pringle, M. S., 2001, Geologic evolution of the Escondida area, northern Chile: a model for spatial and temporal localization of porphyry Cu mineralization: Economic Geology, 96, 271–306.
Scheuber, E., 1990, The kinematic and geodynamic significance of the Atacama Fault Zone, Northern Chile: Journal of Structural Geology, 12(2), 243–257.
Susie, M. E., Guilermo, C. D., David, J. P., and Stephen, S. F., 1996, Structural styles in the Domeyko range, northern Chile: Third ISAG, St Malo (France), 9, 17–19.
Taylor, G. K., Grocott, J., Pope, A., and Randall, D. E., 1998, Mesozoic fault systems, deformation and fault block rotation in the Andean forearc: a crustal scale strike-slip duplex in the Coastal Cordillera of northern Chile: Tectonophysics, 299, 93–109.
Thébault, E., Purucker, M., Whaler, K. A., Langlais, B., and Sabaka, T. J., 2010, The magnetic field of the earth’s lithosphere: Space Sci. Rev., 155, 95–127.
Wang, L., Li, T. C., and Yang, X. Y., 2012, Application of borehole core magnetic susceptibility and PXRF measurement to the Moon mountain copper-iron mining area in Chile and prospecting prediction: Geology and Exploration, 48(2), 396–405 (in Chinese with English abstract).
Wang, W. Y., 2012, Spatial variation law of the extreme value position of analytical signal amplitude for potential field data: Chinese Journal of Geophysics, 55(4), 1288–1299 (in Chinese).
Wang, W. Y., Feng, X. L., Gao, L. J., Wang, P. F., and Liu, B., 2014a, The application of gravity and magnetic techniques to the prospectiong for the Tuerkubanto copper-nickel ore district: Geophysical and Geochemical Exploration, 38(3), 423–429 (in Chinese with English abstract).
Wang, W. Y., Pan, Y., and Qiu, Z. Y., 2009, A new edge recognition technology based on the normalized vertical derivative of the total horizontal derivative for potential field data: Applied Geophysics, 6(3), 226–233.
Wang, W. Y., Wang, Y. P., Li, J. G., Liu, J. L., Zhao, B., and Zhou, X. P., 2014b, Study on the faults structure and granite body distribution in Pangshan area of Yudu-Ganxian ore district using gravity and magnetic data: Geophysical and Geochemical Exploration, 38(4), 825–834 (in Chinese with English abstract).
Wang, W. Y., Zhang, G. C., and Liang, J. S., 2010, Spatial variation law of vertical derivative zero points for potential field data: Applied Geophysics, 7(3), 197–209.
Wei, Y. Q., Ni, W. C., and Fang, J. Q., 2016, The application of the edge enhancement methods to aeromagnetic data processing: Geophysical and Geochemical Exploration, 40(1), 117–124 (in Chinese with English abstract).
Zhang, P., Wang, D. Y., and Zhi, H. N., 2014, A study of tracking the concealed magnetic body in airbone magnetic survey: Geophysical and Geochemical Exploration, 38(1), 1–9 (in Chinese with English abstract).
Zhou, J. F., and Wu, J. T., 1983, Magnetic anomaly and continental volcanic mechanism: Geology and Exploration, 1, 49–56 (in Chinese).
Zhou, L. X., Zhou, J., and Jia, C. S., 2010, The Mesozoic stratabound type copper (sliver) deposits in the coastal range of middle and northern Chile: Mineral Exploration, 1(4), 393–399 (in Chinese with English abstract).
Acknowledgments
The authors thank the reviewers for their constructive comments and suggestions! The authors thank all the people who joined in the acquisition of the aeromagnetic data in the north of Chile!
Author information
Authors and Affiliations
Corresponding author
Additional information
This work was jointly supported by the National Science Foundation of China (No. 41404070) and China Geological Survey (No. DD20160102-02).
Zhu Xiao-San, Ph.D., associate researcher. He received a bachelor’s degree from China University of Mining and Technology in 2002, a master’s degree from China University of Petroleum (Beijing) in 2005 and a Ph.D. degree from Peking University in 2010. His main research interests are acquisition, processing and interpretation of geophysical data and mineral deposits in the Andean metallogenic belt. Contact information: Institute of Geology, Chinese Academy of Geological Sciences. Email: zhuxiaosan@yahoo.com
Lu Min-Jie Ph.D., he graduated Ph.D. degree from Changchun Geological College in 1985. Now he is a Director of Research Center of 3D geology; Institute of geology; Chinese Academy of Geological Sciences. His main research interests are mineral geology and mineral deposits.
Rights and permissions
About this article
Cite this article
Zhu, XS., Lu, MJ. Regional metallogenic structure based on aeromagnetic data in northern Chile. Appl. Geophys. 13, 721–735 (2016). https://doi.org/10.1007/s11770-016-0593-6
Received:
Revised:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11770-016-0593-6