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Updated: Jul 26, 2025

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Watershed Planning within a Quantitative Scenario Analysis Framework
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穆里亚河流域 (里约热内卢部分) 的热结构评估
Suze N P Guimarães1, Fábio P Vieira1, Hellen R Barboza2
1Observatório Nacional (ON/MCTI), Departamento de Geofísica, Laboratório Geotérmico (LabGeot/ON), Rua General José Cristino, 77, São Cristóvão, 20921-400 Rio de Janeiro, RJ, Brazil.
Anais da Academia Brasileira de Ciencias
|June 21, 2023
概括
调查穆里亚河流域的水分.
科学领域:
- 地质物理学 地质物理学
- 地质地质地质地质地质地
- 水文学的水文学
背景情况:
- 水文盆地为地球地的演变提供了洞察力.
- 缓解形式的结果是构造,pedogenic,气候和热过程.
研究的目的:
- 为了评估Muriaé流域的地热场.
- 确定区域构造学特征及其与地热异常的关系.
主要方法:
- 使用了8个热日志和22个地球化学日志.
- 从空中传递的磁性数据中解释了65个磁性线条的表面结构线条以及65个磁性线条.
- 分析的磁体深度高达4.5公里.
主要成果:
- 确定了以北北向南方向的区域构造结构.
- 观察到磁线和地形结构之间的空间相关性.
- 根据磁体深度和热流分布,划出了两个不同的热结构区域.
结论:
- 穆里亚河流域表现出复杂的热结构特征.
- 地质物理和地化学数据揭示了重要的地下地质结构,影响了地热场.
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