山东国土资源
山東國土資源
산동국토자원
LAND AND RESOURCES IN SHANGDONG PROVINCE
2011年
10期
1-6
,共6页
李洪奎%禚传源%耿科%梁太涛%江胜国
李洪奎%禚傳源%耿科%樑太濤%江勝國
리홍규%작전원%경과%량태도%강성국
岩石构造组合%郭家岭花岗闪长岩一花岗岩%胶东地区
巖石構造組閤%郭傢嶺花崗閃長巖一花崗巖%膠東地區
암석구조조합%곽가령화강섬장암일화강암%효동지구
Jiaodong area%granodiorite--granite in Guojialing group%combination of rock structures
通过对前人就郭家岭花岗岩构造地质学、岩石化学、同位素年代学等地质信息资料的分析、研究,认为胶东地区郭家岭花岗闪长岩一花岗岩总体上归属于幔源岩浆与壳源岩浆混合后经分异作用而成的同熔深成型花岗岩类;主要形成于由洋壳俯冲引起的火山岛弧环境、大陆碰撞环境和弧后拉张性质的大陆边缘环境;其定位机制为:沿着NEE向挤压带从小面积到大面积频率式脉动或涌动热轻气球膨胀式定位;该岩石构造组合主体形成于早白垩世。从岩石构造组合的概念,将其定义为造山中期郭家岭弱片麻状花岗闪长岩~花岗岩组合。
通過對前人就郭傢嶺花崗巖構造地質學、巖石化學、同位素年代學等地質信息資料的分析、研究,認為膠東地區郭傢嶺花崗閃長巖一花崗巖總體上歸屬于幔源巖漿與殼源巖漿混閤後經分異作用而成的同鎔深成型花崗巖類;主要形成于由洋殼俯遲引起的火山島弧環境、大陸踫撞環境和弧後拉張性質的大陸邊緣環境;其定位機製為:沿著NEE嚮擠壓帶從小麵積到大麵積頻率式脈動或湧動熱輕氣毬膨脹式定位;該巖石構造組閤主體形成于早白堊世。從巖石構造組閤的概唸,將其定義為造山中期郭傢嶺弱片痳狀花崗閃長巖~花崗巖組閤。
통과대전인취곽가령화강암구조지질학、암석화학、동위소년대학등지질신식자료적분석、연구,인위효동지구곽가령화강섬장암일화강암총체상귀속우만원암장여각원암장혼합후경분이작용이성적동용심성형화강암류;주요형성우유양각부충인기적화산도호배경、대륙팽당배경화호후랍장성질적대륙변연배경;기정위궤제위:연착NEE향제압대종소면적도대면적빈솔식맥동혹용동열경기구팽창식정위;해암석구조조합주체형성우조백성세。종암석구조조합적개념,장기정의위조산중기곽가령약편마상화강섬장암~화강암조합。
Through analysis and study on previous information of granite tectonics, petroclaemlstry, isotope geochronology and other geological information of Guojialing group, it is regarded that granodiorite--granite of Guojialing group in Jiaodong area generally belongs to syntexis plutonic granites which were formed by differentiation after the mixture of mantle--derived magma and crustal magma. It was mainly formed by volcanic island arc environment, continental collision and back--arc extensional environment casued by the subduction of oceanic crust. Its positioning mechanism is as follows: small square to large square of squee- zing belts with the trend of NNE frequency pulse type or magma swelling hot--air balloon expandable positioning. This combination body was formed in early Cretaceous. From the concept of rock combination, it is defined as the Guojialing weak gneissic granodiorite and granite combination in middle orogenic period.