CAJ | 학술논문

关于锡林郭勒杂岩，前人有两种相异观点[1-4]，一种认为，它是由深成岩体受剪切作用变形变质而形成的正变质岩，其形成于早古生代；另一种认为它是由碎屑岩-火山岩经过区域动力变质作用形成的副变质岩，时代属于前寒武。本文通过研究认为锡林郭勒杂岩之中各类岩石具有相同的变质变形特征，互层关系稳定，是一套连续的岩层，原岩应为滨浅海碎屑沉积夹基性、中基性火山岩建造。锡林郭勒杂岩的变质年龄揭示了一次重要构造运动，标志着华北板块北缘结束元古代陆缘发育进入古生代发展。
관우석림곽륵잡암，전인유량충상이관점[1-4]，일충인위，타시유심성암체수전절작용변형변질이형성적정변질암，기형성우조고생대；령일충인위타시유쇄설암-화산암경과구역동력변질작용형성적부변질암，시대속우전한무。본문통과연구인위석림곽륵잡암지중각류암석구유상동적변질변형특정，호층관계은정，시일투련속적암층，원암응위빈천해쇄설침적협기성、중기성화산암건조。석림곽륵잡암적변질년령게시료일차중요구조운동，표지착화북판괴북연결속원고대륙연발육진입고생대발전。
There are two different views about Xilin Gol metamorphic assemblage. one that is deep into the rock by its shear deformation and metamorphic rocks are formed, which was formed in the early Paleozoic;second is that it is a clasticrock-volcanic rocks After the formation of the regional dynamic metamorphism Vice metamorphic rocks belong to the Precambrian era. This practice areas based on findings, researchers believe that The various types of rocks in Xilin Gol metamorphic assemblage have the same deformation characteristics, Interbedded relations are stable level, is a continuous rock, protolith rock should be the littoral and shallow marine clastic sedimentary, folder neutral and basic volcanic rocks.