Sticking together:Mechanisms of quartz synneusis in high-silica magma  

作　　者：Brendan Dyck 

机构地区：[1]Department of Earth,Environmental and Geographic Sciences,The University of British Columbia,4237 University Way,Kelowna,BC V1V 1V7,Canada

出　　处：《Geoscience Frontiers》2023年第2期40-46,共7页地学前缘（英文版）

摘　　要：The formation of crystal clusters by synneusis(magmatic sintering)affects a wide range of magmatic systems from olivine clusters in komatiite to quartz clusters in high-silica granite.A common feature of synneusis in any mineral phase is the alignment of neighbouring crystals in certain lower-energy orientation relationships.However,the underlying mechanisms involved with both the alignment of crystals in lower-energy orientations and the binding of crystal clusters are not well understood.In the absence of mechanisms that bind crystals together upon contact,the same hydrodynamic forces that may bring crystals together can in theory also serve to disaggregate clusters.Here I use cathodoluminescence imaging and crystal orientation data from quartz clusters in high-silica granite to show that i)rapid crystalline neck growth along attachment surfaces and ii)grain rotation are two mechanisms that reduce the grain boundary energy of crystal clusters while increasing clusters’shear strength.The continued crystallization of sintered phases as the magmatic body cools further cements crystal pairs and resists cluster disaggregation.Together these mechanisms underpin both the formation and preservation of large crystal clusters in dynamic magmatic environments.

关 键 词：Synneusis GRANITE Magmatic behaviour EBSD CATHODOLUMINESCENCE QUARTZ 

分 类 号：P611[天文地球—矿床学]