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Interpretation of high resolution aeromagnetic data for structures study and exploration of polymetallic deposits in Kalatage area, eastern Tianshan (NW China)

机译:浅析天山市喀土地区高分辨率气动数据的结构研究与探索(NW中国)

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摘要

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 theta map 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.
机译:进行了高分辨率的Kalatage地区的航空磁性调查,旨在提供详细的地质结构信息和引导进一步的矿物勘探。处理最近获得的数据并解释为更好地理解Cu-Au多金属沉积物的发生模式和相关的结构特征。若干分析技术,例如降低到极点,光谱分析,低通滤波,用于处理气磁数据以了解磁性源的分布。通过光谱分析估计磁性源的深度,分析较浅和更深的源异常。欧拉去卷积,总水平衍生物,倾斜角衍生物和θ地图用于研究谱系结构。通过比较高于Kalatage地区的衍生结果和地质数据来确定新的结构方案。结果表明,研究区受到NWW-SEE / NW-SE,NNE-SSW / NE-SW和几乎E-W方向故障结构的影响;各种可能的岩石岩石可能是沿着这些区域骨折在大规模和深刻的构造 - 岩浆活动过程中的上升和侵入岩浆的结果。多金属矿石沉积物主要分布在研究区域的东部部分内,并且可能沿着结构界面局限于建议它是在结构上控制的。此外,提出了矿化的有利区域。这些分析有助于识别不同磁化的结构特征,对构造演化的解释,这可能对进一步的矿物勘探具有重要参考。

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