| “构造附加静水压力”及其应用 |
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| 引用本文： | 吕古贤,周绍东,文锦明,杨恒书.“构造附加静水压力”及其应用[J].四川地质学报,1999(2). |
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| 作者姓名： | 吕古贤 周绍东 文锦明 杨恒书 |
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| 作者单位： | 地质力学研究所，四川地勘局 |
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| 基金项目： | 国家计委科技找矿项目,国家科委基础研究特别支持项目,国家攀登项目 |
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| 摘 要： | 提出地壳任一点静水压力部分是由重力所附加的静水压力和由构造作用力所附加的静水压力叠合而成的。处在挤压变形带、剪切变形带到引张变形带（及地域）中岩石所承受的构造附加静水压力有逐次变小的规律性。构造叠加致使同一地壳深度的水平面上静水压力值不相等，这种压力梯度是流体及油气长距离水平运移的主要原因。建立岩石矿床形成深度的构造校正测算方法，并提出构造物理化学成矿的新认识。
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| 关 键 词： | 构造附加静水压力 成矿深度的构造 校正测算 构造物理化学 |
TECTONIC SUPERIMPOSED HYDROSTATIC PRESSURE AND ITS APPLICATION |
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| Abstract: | Hydrostatic pressure at a point in crust is composition of gravity superimposed hydrostatic pressure and tectonic superimposed hydrostatic pressure.There is a gradual decrease in tectonic superimposed hydrostatic pressure from compressional deformation zone through shear deformation zone to extensional deformation zone.Tectonic superimposition results in hydrostatic gradient at the same level which is responsible for migration of fluids including oil and gas.A tectonically corrected calculus of ore forming depth and tectonically controlled physical chemical ore formatim are put forward. |
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| Keywords: | tectonic superimposed hydrostatic pressure tectonically corrected calculus of ore forming depth tectonic physicochemistry |
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