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논문 기본 정보

자료유형
학술저널
저자정보
Shaole An (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences) Kefa Zhou (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences) Jinlin Wang (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences) Nannan Zhang (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences) Shibin Liao (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences) Qianwen Feng (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences) Zhixin Zhang (Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences)
저널정보
한국지질과학협의회 Geosciences Journal Geosciences Journal Vol.24 No.3
발행연도
2020.1
수록면
315 - 327 (13page)

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A high resolution aeromagnetic survey of Kalatage area was carried out, aimed at providing detailed geological structures information and guiding for further mineral prospecting. The recently acquired data was processed and interpreted to better understand the mode of occurrence of the Cu-Au polymetallic deposits and associated structural features. Several analysis techniques, such as reduction to the pole, spectral analysis, low-pass filtering, were applied to process the aeromagnetic data to understand the distribution of magnetic sources. The depth of magnetic sources was estimated by spectral analysis, and the shallower and deeper sources anomalies were analyzed. The Euler deconvolution, total horizontal derivative, tilt angle derivative and thetamap were used to study lineament structures. The new structural scheme was established by comparison of above derivative results and geological data of the Kalatage area. The results show that the study area is affected by sets of NWW-SEE/NW-SE, NNE-SSW/NE-SW and nearly E-W directions faults structures; various probable magmatic rocks may be the results of the ascent and intrusion of magma along these regional fractures in the process of large-scale and deep tectonic-magmatic activities. The polymetallic ore deposits are mainly distributed within the eastern portion of the study area and are confined probably along structure lineament suggesting that it is structurally controlled. Furthermore, the favorable area for mineralization was proposed. These analyses help the recognition of structure features of differing magnetizations, interpretation of tectonic evolution, which could have important reference for further mineral prospecting.

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