Geological interpretation of Bouguer gravity and aeromagnetic data from the Gobi-desert covered area, Eastern Tianshan, China: Implications for porphyry Cu-Mo polymetallic deposits exploration
Geological interpretation of Bouguer gravity and aeromagnetic data from the Gobi-desert covered area, Eastern Tianshan, China: Implications for porphyry Cu-Mo polymetallic deposits exploration
复制标题
中国东天山戈壁沙漠覆盖区布格重力和航磁数据的地质解释:对斑岩铜钼多金属矿床勘探的启示
DOI:
10.1016/j.oregeorev.2016.08.034
复制
发表时间:
2017
影响因子:
3.3
通讯作者:
Zhenghai Wang
中科院分区:
文献类型:
--
作者:
Fan Xiao;Zhenghai Wang
In this study, Bouguer gravity and aeromagnetic data have been used to better understand the geology and mineral resources near the late Carboniferous-late Permian porphyry Cu-Mo polymetallic mineralization in the Chinese Eastern Tianshan belt, which is extensively covered by Gobi-desert. The reduced-to-pole (RTP) transformation of regional-scale aeromagnetic data shows that the porphyry Cu-Mo deposit is within a cluster of magnetic anomaly highs that overprint on a northeast trending magnetic gradient belt generally along the crustal-scale Kanguertag-Huangshan fault. The 10 km upward continuation transformation of both Bouguer gravity and aeromagnetic data indicates that the known porphyry Cu-Mo polymetallic deposits are located on the flanks of prominent gravity and magnetic anomaly highs. These anomalies are spatially correlated with the late Carboniferous-late Permian igneous rocks and in the Tuwu-Yandong mineralization district are centered over the granodiorite rocks genetically related to porphyry copper systems. In order to minimize interpretational ambiguities, a useful approach that is correlation analysis (CA) based on correlation coefficient (CC) given by gravity and magnetic data was employed to separate positively and negatively correlated anomalies features. The CA procedure is applied to 10 km upward continuation transformation of both Bouguer gravity and RTP transformed aeromagnetic data for mapping correlative magnetization and density contrast anomalies from deep sources, which may be associated with the porphyry Cu-Mo polymetallic mineralization. Five prominent CC positive anomalies have been found in the southern margin of Dananhu-Tousuquan arc. Those anomalies zones could be interpreted to reflect a late Carboniferous-late Permian magmatic belt that is favorable for additional discoveries of late Carboniferous to late Permian porphyry copper systems in north region of Eastern Tianshan.
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DOI:
--
发表时间:
2013
期刊:
The Journal of Geology
影响因子:
--
作者:
Zeng Ka
通讯作者:
Zeng Ka
影响因子:
3.5
作者:
Taofa Zhou;F. Yuan;Yu Fan;Dayu Zhang;D. Cooke;Guochun Zhao
通讯作者:
Taofa Zhou;F. Yuan;Yu Fan;Dayu Zhang;D. Cooke;Guochun Zhao
DOI:
10.1007/978-94-007-0406-0
发表时间:
2011-12
期刊:
Bouguer Gravity Regional and Residual Separation: Application to Geology and Environment
影响因子:
--
作者:
K. Mallick;A. Vasanthi;K. K. Sharma-K.
通讯作者:
K. Mallick;A. Vasanthi;K. K. Sharma-K.
影响因子:
3.3
作者:
Chunming Han;W. Xiao;Guochun Zhao;J. Mao;Jianmin Yang;Zhiliang Wang;Zhen Yan;Q. Mao
通讯作者:
Chunming Han;W. Xiao;Guochun Zhao;J. Mao;Jianmin Yang;Zhiliang Wang;Zhen Yan;Q. Mao
DOI:
--
发表时间:
2005
期刊:
Acta Geological Sinica
影响因子:
--
作者:
Chen Fuwen
通讯作者:
Chen Fuwen