摘要
吉林省中部,在伊通—依兰与敦化—密山断裂带之间,北起舒兰红石砬子,循近南北方向,南入蛟河拉法;一支转向永吉—伊通;一支转向敦化青沟子—朱敦店;一支顺永吉—呼兰镇的两侧,即桦甸常山—富太河;磐石红石砬子—新锅盔山;发育了一条空间展布形态独具特色的A型花岗岩带。它形成的时代为230Ma左右。这是松(松嫩)—佳(佳木斯)—龙(龙岗)三个地块之间的活动带,从新元古代演化发展,由过渡型陆壳转化为成熟陆壳,结束其“古吉黑造山带”历史的重要标志。
Between Yitong Yilan and Dunhua-Mishan faUlted zones in the central part of Jilinprovince,A-type granite zone with the unique characteristic is distributed as the followingextent,i.e.,from Hongshilazi,Sulan county in the north to Lafa,Jiaohe county in the south;from Yongji to Yitong;from Qinggouzi,Dunhua county to Zhudundian(from Changshan,Huadian county to Futai River);from Hongshilazi,Panshi county to Xinguokuishan. Theforming age is about 230Ma. this belongs to active zone which joins along the Songnen,Jia-musi and Longgang blocks. Since the Proterozoic,the transition-type continental crust hasbeen developed to mature continental crust,forming Paleojihei orogenic belt.
出处
《吉林地质》
1995年第3期31-44,共14页
Jilin Geology
关键词
A型花岗岩
陆壳演化
花岗岩
构造意义
A type granite Mark of continental evolution The central part of Jilinprovince