在白纪晚期的德坎 magma 和喷发式气体释放中的硫和
Stephen Self1, Stephen Blake, Kirti Sharma
1Volcano Dynamics Group, Department of Earth and Environmental Sciences, Open University, Milton Keynes MK7 6AA, UK. stephen.self@open.ac.uk
概括
来自印度的大规模古老的岩流.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 古气候学 古气候学
背景情况:
- 印度的德坎陷是由6.7-65亿年前的大批帕霍霍岩流形成的.
- 这些洪水玄武岩喷发对大气和灭绝的影响仍然不确定.
研究的目的:
- 为了评估Deccan Traps火山活动可能释放的气体.
- 量化硫 (S) 和 (Cl) 的排放量.
主要方法:
- 测量了德坎岩内的玻璃内含物和野中的S和Cl度.
- 计算出每次喷发的岩体积的潜在SO2和HCl气体释放量.
主要成果:
- 德坎岩的S度在数百至1400ppm之间;Cl度高达900ppm.
- 喷发可能释放高达5.4 Tg SO2/km3和1 Tg HCl/km3.
- 保守的估计表明3.5 Tg SO2/km3和1 Tg HCl/km3.
结论:
- 德坎陷喷发释放了大量的S和Cl气体.
- 严重的环境影响很可能是这些大规模的洪水玄武岩事件造成的.
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