有证据表明,岩由火成体烧结而形成的岩
Annabelle Foster1, Fabian B Wadsworth2, Hugh Tuffen3
1Earth Science, Durham University, Science Labs, Durham, DL1 3LE, UK. annabelle.foster@durham.ac.uk.
Nature communications
|June 24, 2024
概括
岩岩由火山灰在喷发前在地下烧结而形成. 这项研究揭示了冰岛这一过程的证据.
科学领域:
- 火山学 火山学是一门学科.
- 伊格尼岩石学 伊格尼岩石学
- 地质化学 地质化学
背景情况:
- 岩可能起源于地下火成体烧结和随后的通风引流.
- 了解状火山管道的形成机制对于喷发动态至关重要.
- "密码碎片化模型"提出了一种流动性岩火山运动的途径.
研究的目的:
- 为火成体的烧结提供证据,作为形成岩的机制.
- 研究冰岛克拉夫拉火山Hrafntinnuhryggur火山保护的火山管道系统.
- 分析管道纹理,岩脱气和喷发沉积物之间的关系.
主要方法:
- 现场观测和地质绘制暴露的火山管道.
- 管道边缘沉积物的岩石学分析,包括石灰石,石灰,石灰和石灰.
- 在管道中实地测量H2O度,以评估岩脱气模式.
主要成果:
- 管道边缘显示了从石支的石灰岩皮岩岩岩到密集的黑色灰的过渡.
- 氧化样本含有遗迹石块边界和石质碎片,表明在管道中烧结.
- 在H2O度的横向变化表明渐进的管道堵塞和气体加压.
结论:
- 这项研究提供了强有力的证据,支持在岩形成中的火成体的地下烧结.
- 在Hrafntinnuhryggur的暴露管道保存了岩脱气和管道过程的记录.
- 这些发现支持了"密码碎片化模型"对流动性岩火山的支持.
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