Textures and melt-crystal-gas interactions in granites

作     者：Jean-Louis Vigneresse 

作者机构：GeoRessourcesUMR 7339Universite de Lorraine 

出 版 物：《Geoscience Frontiers》 (地学前缘（英文版）)

年 卷 期：2015年第6卷第5期

页      面：635-663页

核心收录：

学科分类：0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 0708[理学-地球物理学] 0704[理学-天文学] 

主　　题：Granitic magma Instabilities Triclinic flow Struct 

摘      要：Felsic intrusions present ubiquitous *** result from the differential interactions between the magma components(crystal,melt,gas phase) while it flows or when the flow is perturbed by a new magma *** most obvious structure consists in fabrics caused by the interactions of rotating grains in a flowing viscous *** magma inputs through dikes affect the buk massif flow,considered as global within each mineral facies.A review of the deformation and flow types developing in a magma chamber identifis the patterns that could be *** determines their controlling parameters and summarizes the tools for their ***,a brief review of the theology of a complex multiphase magma identifies and suggests interactions between the different *** specific responses each component presents lead to instability *** particular,the change in vorticity orientation,associated with the switch between monoclinic to triclinic flow is a cause of many *** are preferentially *** include fabric development,shear zones and flow *** depend of the underlying rheology of interacting ***,enclaves,schlieren and ladder dikes result from the interactions between the magma components and changing boundary ***,pegmatites,unidirectional solidification textures and miarolitic cavities result from the interaction of the melt with a gaseous *** illustrations examine what is relevant to the bulk flow,local structures or boundary *** each case a field observation illustrates the *** discussion reformulates instability observations,suggesting new trails for ther description and interpretation in terms of local departure to a bulk flow.A brief look at larger structures and at their evolution tries to relate these instabilities on a broader *** helical structures of the Ricany pluton,Czech Republic and by the multiple granitic intrusions of Dolbe