| 埋藏条件下碳酸盐岩实验室溶蚀作用模拟的热力学模型与地质勘探方向——以陕甘宁盆地下奥陶统马家沟组第五段为例 |
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| 引用本文： | 肖林萍.埋藏条件下碳酸盐岩实验室溶蚀作用模拟的热力学模型与地质勘探方向——以陕甘宁盆地下奥陶统马家沟组第五段为例[J].沉积与特提斯地质,1997,17(4):57-70. |
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| 作者姓名： | 肖林萍 |
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| 作者单位： | 长春科技大学能源地质系 |
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| 摘 要： | 地热流体是沉积岩孔隙空间中的流体，这里提出的地热流体这一术语，是用来描述通过地球中孔隙空间的流体。本文讨论了地面和大气水流、压实流、对流和孔隙流体。
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| 关 键 词： | 地热流体 压实流 对流 孔隙流体 |
THERMODYNAMIC MODEL FOR EXPERIMENTAL SIMULATION OF DISSOLUTION OF THE CARBONATE ROCKS IN THE BURIAL ENVIRONMENTS:AN EXAMPLE FROM THE FIFTH MEMBER OF THE LOWER DEVONIAN MAJIAGOU FORMATION IN THE SHAANXI-GANSU-NINGXIA BASIN |
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| Xiao Linping.THERMODYNAMIC MODEL FOR EXPERIMENTAL SIMULATION OF DISSOLUTION OF THE CARBONATE ROCKS IN THE BURIAL ENVIRONMENTS:AN EXAMPLE FROM THE FIFTH MEMBER OF THE LOWER DEVONIAN MAJIAGOU FORMATION IN THE SHAANXI-GANSU-NINGXIA BASIN[J].Sedimentary Geology and Tethyan Geology,1997,17(4):57-70. |
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| Authors: | Xiao Linping |
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| Institution: | Xiao Linping Southwest China Jiatong University |
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| Abstract: | Geofluids are fluids through pore spaces in the sedimentary rocks.This paper presents a discussion of geofluids as a term which has been used to describe the fluids through pore spaces in the Earth.Ground and meteoric water flow,compactional flow,convection current and pore fluids have been discussed in this paper. |
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| Keywords: | experimental simulation carbonate rock Shaanxi Gansu Ningxia Basin Gibbs free energy |
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