Geochemistry of volcanics and fluid-rock interactions in hydrothermal systems in the Manus Basin

东马努斯盆地（EMB）是世界上板块构造最活跃和地球化学最多样化的地区之一。马努斯盆地的许多火山中心都有热液系统，这些热液系统不同程度地受到岩浆脱气的影响。这些系统的地球化学多样性提供了一个无与伦比的机会来研究岩浆脱气及其对热液系统中物质运输的影响。在最近的一次RV Melville巡航中，在EMB的不同区域收集了火山岩、热液流体和硫化物。岩石覆盖范围从枕状玄武岩到高度泡状的长英质熔岩，其中一些是高度斑岩。流体排出区附近的岩石蚀变也变化很大，从泥质到酸硫酸盐蚀变不等。这些样品将有助于评估岩浆组分输入热液系统的岩浆分异，以及对流体-岩石相互作用和金属运输的影响。在模型计算中，将热液活动区新鲜岩石和蚀变岩石的地球化学数据与喷口流体的化学分析相结合，以解释(1)观察到的相组合和(2)喷口流体化学。我们将使用反应路径模型来模拟岩浆组分可变输入的流体-岩石相互作用。这些结果将与nsf资助的伙伴项目的数据相结合，以便全面了解马努斯盆地岩浆-热液系统的质量传递。

The eastern Manus Basin (EMB) is one of world’s most plate-tectonically active and geochemically diverse regions. Many volcanic centers in the Manus Basin host hydrothermal systems that are affected by magma degassing to variable extent. The geochemical diversity of these systems provides an unparalleled opportunity to examine magma degassing and its consequences for mass transport in hydrothermal systems. During a recent RV Melville cruise volcanic rocks as well as hydrothermal fluids and sulfides were collected in different areas of the EMB. The rocks cover a range from pillow basalt to highly vesicular felsic lava, some of which are highly porphyritic. Rock alteration in the immediate vicinity of the fluid discharge area is also strongly variable, ranging from argillaceous to acid-sulfate alteration. These samples will allow the assessment of magmatic differentiation in relation to input of magmatic components into the hydrothermal system and consequences for fluid-rock interactions and metal transport. Geochemical data of fresh and altered rocks from hydrothermally active areas will be combined with chemical analyses of vent fluids in model calculations aimed at explaining (1) the phase assemblages observed and (2) the vent fluid chemistry. We will use reaction path models to simulate fluid-rock interactions with variable input of magmatic components. The results will be combined with data from NSF-funded companion projects in order to obtain a comprehensive understanding of mass transfers in the Manus Basin magmatic-hydrothermal systems.