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营口—宽甸地区重力场特征及地质解释
引用本文:曹恩久.营口—宽甸地区重力场特征及地质解释[J].国土资源,1991(4).
作者姓名:曹恩久
作者单位:辽宁省地质矿产局物探大队 沈阳
摘    要:营口—宽甸地区重力场自北而南有逐渐增高的总趋势。中部区重力低与重力高呈带状相间出现。结合该区已知的地质构造特征综合分析,重力负值带是早元古宙拗拉槽边界深断裂和构造—岩浆岩带的反映。隐伏、半隐伏花岗岩体的解释和推断,为逃一步寻找金、硼、铅锌等矿产提供了信息。

关 键 词:营口  宽甸  重力场  隐伏岩体  金硼  铅锌

THE CHARACTERISTICS OF GRAVITATIONAL FIELD FROM YINGKOU TO KUANDIAN WITH THE GEOLOGICAL INTERPRETATION
Chao Enjiu The Geophysical Prospecting Team,Liaoning Bureau of Geology and Mineral Resources,Shenyang.THE CHARACTERISTICS OF GRAVITATIONAL FIELD FROM YINGKOU TO KUANDIAN WITH THE GEOLOGICAL INTERPRETATION[J].Land & Resources,1991(4).
Authors:Chao Enjiu The Geophysical Prospecting Team  Liaoning Bureau of Geology and Mineral Resources  Shenyang
Abstract:The gravitational field from Yingkou to Kuandian gradually increases in total from north to south,but in the central area,lower gravitational field alternating with higher field in belt.Considering the known synthetical studies on the characteristics of geological structures,the negative gravitational belt is considered to be a deep fracture or a tectonicmagmatic belts.The interpretation and deduction of concealed,half-concealed granite bodies provide information for looking for gold,boron,lead-zinc deposits.
Keywords:Yingkou Kuandian  Gravitational field  Concealed rock body  Gold Boron  Lead Zinc  
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