粘土 - 硫酸盐平面图转变的诊断,夏普山群,盖尔坑,火星
1Department of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA.
概括
盖尔火山口的基因结构显示了多个流体流动事件. 纹理变化与岩石化学和层级学相关,表明地下地下地下水重新调动了硫酸盐.
科学领域:
- 地质地质地质地质地质地
- 天文地质学 天文地质学
- 沉积物学的沉积物学
背景情况:
- 盖尔火山口的平分层记录显示了粘土-硫酸盐过渡时期独特的基因结构.
- 了解这些纹理可以了解火星过去的水性环境.
研究的目的:
- 通过MAHLI仪器观察到的对基因纹理进行目录和分析.
- 为了建立一个对代遗传序列的diagenetic过程.
- 为了将纹理变化与层级统计单位和大质量岩石化学相关联.
主要方法:
- 使用MAHLI仪器对基因结构 (丰度,形态,交叉关系) 进行分类.
- 分析纹理分布中的空间异质性.
- 与散装岩石化学相关联的结节丰度 (阿尔法粒子X射线光谱仪).
主要成果:
- 识别了多个代谢性流体流动的情节,负责纹理,如颜色变化,坑,结节和Ca-硫酸盐静脉.
- 观察到的纹理多样性的空间变化与分层学单位,粒度大小和压缩有关.
- 连接硫酸盐含量增加的上截面到毛孔填充的代谢性水泥.
结论:
- 盖尔火山口的基因结构表明了复杂的流体流动历史.
- 平流体和岩石特性影响了对遗传特征的分布.
- 地下地下水的重新调动是硫酸沉的合理机制.
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