中文摘要:作者通过分析不同地形_地质界面间的差值域分布特征，对浅层隐伏岩 体进行了数值模拟和产状预测。模拟结果显示铜陵矿集区有可能存在着一个顶点朝下的圆锥 状岩浆构造，从整体上看，该隐伏岩体在深处收缩为一个点源，从该点源往上分布范围逐渐 扩大，岩体也开始发生分叉现象，使靠近或出露于地表的分支岩体在产状上更接近于小型岩 枝。推断它有可能是连接深_浅部之间的岩浆“汇”，该岩浆“汇”将来自更深部岩浆源的 含矿物质和热能转送到更浅部的各分叉岩枝内，并因此成为铜陵矿集区成矿物质的重要来源 和能量来源。
Abstract:The gravity aeromagnetic anomaly and the specific structural assemblage shown in TM images indicate the existence of a shallow concealed magma chamber in the ce nter of Tongling area. Nevertheless, the 3D shape of the concealed magma chamber and its spatial relation with the outcropped apophyses are still not clear. Bas ed on field and drill hole data obtained from Tongling area, the authors carried out a numerical simulation to probe into the difference domain between two stra ta or between the strata and the topographic surface. Moreover, the difference d omain that represents the space filled with the magmatic body was applied to pre dict the subsurface concealed magmatic bodies and analyze their spatial structur es. The results of the numerical simulation show the existence and the 3D shape of a hidden conical magmatic structure beneath the middle of this area. Its top bifurcates southwards into several branches, while its lower part stretches nort heastwards and contracts rapidly to one point. This point is considered to be th e “sink" of the concealed magmatic system, which transfers ore materials and he at energy from the deeper magma chamber to the subsurface apophyses.
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基金项目:国土资料部科技专项计划(编号：20010103)、教育部科学技术研究重点项目(编号 ：03678和01037)、国家自然科学基金重点项目(批准号：40234051)和国家重点基础研究发展规划项目(编号：1999043206)
引用文本：
王庆飞，邓 军，黄定华，张 强.2004.铜陵矿集区浅层隐伏岩体预测及其形态分析[J].矿床地质,23(3):405~410.2004.Prognosis and Morphological Analysis of Subsurface Concealed Magmatic Bodies i n Tongling Ore Concentration Area [J].Mineral Deposits23(3):405~410
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