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    姜枚, 杨经绥, 张聿文, 谭捍东, 彭淼, 吴良士, 许乐红, 张立树, 李庆庆. 西藏泽当岩体含铬超镁铁岩体的深部构造特征与找矿前景探讨[J]. 中国地质, 2013, 40(3): 780-789.
    引用本文: 姜枚, 杨经绥, 张聿文, 谭捍东, 彭淼, 吴良士, 许乐红, 张立树, 李庆庆. 西藏泽当岩体含铬超镁铁岩体的深部构造特征与找矿前景探讨[J]. 中国地质, 2013, 40(3): 780-789.
    JIANG Mei, YANG Jing-sui, ZHANG Yu-wen, TAN Han-dong, PENG Miao, WU Liang-shi, XU Le-hong, ZHANG Li-shu, LI Qin-qin. Deep tectonic characteristics and ore-prospecting potential of the Zetang Cr-bearing ultramafic rock mass in Tibet[J]. GEOLOGY IN CHINA, 2013, 40(3): 780-789.
    Citation: JIANG Mei, YANG Jing-sui, ZHANG Yu-wen, TAN Han-dong, PENG Miao, WU Liang-shi, XU Le-hong, ZHANG Li-shu, LI Qin-qin. Deep tectonic characteristics and ore-prospecting potential of the Zetang Cr-bearing ultramafic rock mass in Tibet[J]. GEOLOGY IN CHINA, 2013, 40(3): 780-789.

    西藏泽当岩体含铬超镁铁岩体的深部构造特征与找矿前景探讨

    Deep tectonic characteristics and ore-prospecting potential of the Zetang Cr-bearing ultramafic rock mass in Tibet

    • 摘要: 提要:在中国最大的铬铁矿罗布莎周边地区有着数目众多的含铬超镁铁岩体;分布广阔,具有很好的找矿前景,选择泽当岩体进行了重、磁、大地电磁法的剖面探测,结果表明:泽当岩体被近南北向断裂切割成多块,其西端岩体向北推移的距离远于东段的岩体,总体上呈北西西向展布;岩体磁异常由蛇纹石化产生的磁铁矿和岩体生成时剩余磁化引起,磁异常指出了岩体浅部的范围;航磁较大范围的异常表明存在较深部的磁性体;重力异常说明岩体局部存在高密度体,且与磁异常相吻合,地表出露的矿点多分布在此范围内;岩体表层为高阻薄层,在剖面中段高阻体厚度最大处达1.5 km,范围不大。在薄高阻体下为薄层低阻层。电阻率剖面两侧以高阻体为主,中段有多个低阻体,且与深部5~25 km深度上的低阻体相连,中地壳范围的低阻体与幔源物质上涌在地壳范围留下的熔融体有关,与地壳上部的超镁铁岩体有关。综合各种地球物理场的特征认为在磁异常分布区内具有局部重力异常、低阻体异常较多的地段是泽当岩体最有利于进一步详细探测找矿的部位。

       

      Abstract: Abstract:Numerous Cr-bearing ultramafic rock masses with high ore-prospecting potential are distributed around Luobusha, the largest chromite deposit in China. The Zetang rock mass was selected to conduct profile probing using gravimetric, magnetic and magnetotelluric methods. The results show that the Zetang rock mass was cut into several parts by approximately NS-trending faults, with the west parts moving farther northward than the east ones and distributed in NWW directions on the whole. The magnetic anomalies in the mass were caused by the magnetite resulting from the serpentinization and the residual magnetization when the rock mass was formed, and such magnetic anomalies indicate the limits of the superficial part of the rock mass. The gravity anomalies reveal that there are high-density bodies existing locally in the mass, which accord with the magnetic anomalies, and the outcropped ore spots at the earth's surface are mostly distributed within the limits. The surface layer of the mass is a thin high-resistance layer, with a thickness of at least one hundred meters in general, and the maximum thickness of the high-resistance body reaches 1.5 km in the middle section of the mass profile but its area is not large. Under the thin high-resistance bodies, there is a thin low-resistance layer. Both sides of the profile are dominated by high-resistance bodies, but the middle section contains quite a few low-resistance bodies, which are connected with the low-resistance bodies in the deep part at the depth of 5–25 km and thus belong to the low-resistance bodies in the middle crust. It is inferred that these low-resistance bodies were caused by partial melting, suggesting that there probably existed passages for the upward migration of mantle-derived materials. Through summarizing the characteristics of various geophysical fields, it is thought that the sectors with more local gravity anomalies and low-resistance body anomalies in a magnetic anomaly area are most favorable for further detailed exporation and ore-prospecting work.

       

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