玛射线元素在Cerro do Jarau冲击结构中的分布和地热建模提案
Diego D Garcia1, Emilson P Leite1, Marcos Alberto R Vasconcelos2
1Universidade Estadual de Campinas, Instituto de Geociências, R. Carlos Gomes, 250, Cidade Universitária, 13083-855 Campinas, SP, Brazil.
Anais da Academia Brasileira de Ciencias
|March 21, 2024
概括
石撞击导致岩石变形和流体循环. 这项研究使用放射测量数据和模拟分析了Cerro do Jarau冲击结构,揭示了与冲击后的热水活动相关的液体移动.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 行星科学 行星科学
背景情况:
- 大型石撞击会产生大量的动能,导致岩石变形,高温和流体循环.
- 了解冲击后的热水流及其与当地地质学的关系对于描述冲击结构至关重要.
研究的目的:
- 调查Cerro do Jarau冲击结构内岩石变形和流体循环之间的相关性.
- 描述撞击结构中元素 (K,eTh,eU) 的放射学特征和空间分布.
- 模拟流体循环模式,了解后期的热水过程.
主要方法:
- 收集和分析地面马射线数据以确定K,eTh和eU度.
- 生成放射性地图 (eTh/K比,F-因子) 以可视化空间分布.
- 使用HYDROTHERM 3代码进行数值模拟,以建模流体循环模式.
主要成果:
- 放射测量数据显示,K,eTh和eU度从外围边缘向火山口的中心普遍下降.
- 中部地区的放射值非常低,度相对较高,暗示存在含有K的岩石.
- 数字模拟显示了撞击结构内的特定流体循环模式.
结论:
- 放射测量和模拟数据表明,Cerro do Jarau冲击结构内的流体可能会重新调动.
- 水热过程可能在火山口形成过程的后期阶段发挥了作用.
- 该研究提供了对撞击诱导变形和地质环境中的流体动力学之间的相互作用的见解.
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