摘要
<正>蛇纹石一种富水矿物,其水含量高达13.5 wt%,常见化学式为Mg3Si2O5(OH)4,但实际上蛇纹石中会富集铁、铝等元素。蛇纹石主要是由超基性岩(科马提岩、橄榄岩等)和富水流体反应形成,这个反应是蛇纹石化作用。蛇纹石化广泛分布于多种构造环境中,主要包括洋底、慢速扩张洋中脊和俯
引文
Barnes,J.D.,Sharp,Z.D.2006.A chlorine isotope study of DSDP/ODP serpentinized ultramafic rocks:insights into the serpentinization process.Chemical Geology 228,246-265.
Scambelluri,M.,Fiebig,J.,Malaspina,N.,Müntener,O.,Pettke,T.,2004.Serpentinite subduction:implications for fluid processes and trace-element recycling.International Geology Review 46,595-613.
Sharp,Z.D.,Barnes,J.D.2004.Water-soluble chlorides in massive seafloor serpentinites:a source of chloride in subduction zones.Earth and Planetary Science Letters 226,243-254.