Peculiarities of the Absk Intrusion Traps and Their Formation Conditions (Siberian Platform)
Results of petro-geochemical investigations of the Absk intrusion traps in the southern Siberian platform are presented.The presence of dolerite varieties with relatively high alkaline and silica contents is characteristic of the Absk intrusion traps.Occurrence of high alkaline rock varieties is related to different structural position of the magma conducting faults relative to magma chamber and fluid reworking of rocks as well as to local postmagmatic influence of residual deep fluid on initial dolerites.It is suggests that the plume-lithosphere interaction was the mechanism by which the Absk intrusion was formed within the trap province.
basic rocks magmatism sills traps Siberian platform
M.E.Tonkikh K.N.Egorov A.I.Kiselev
National Research Irkutsk State Technical University,Irkutsk,Russia Institute of the Earths crust,Irkutsk,Russia
国际会议
第十八届凯洛林国际地质学术研讨会(The 18th Kerulien International Conference on Geological)
石家庄
英文
411-415
2013-09-20(万方平台首次上网日期,不代表论文的发表时间)