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地质论评  2011 

黑龙江杂岩带的形成演化及地质意义

Keywords: 黑龙江杂岩带,嘉荫―牡丹江缝合带,佳木斯地块,松嫩地块,中国东北,古亚洲洋南支

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Abstract:

黑龙江杂岩带呈南北向带状展布于佳木斯地块西缘,出露于嘉荫―牡丹江缝合带以东。研究证明其主体形成时代为晚海西期到印支期,地球化学特征显示其极可能形成于佳木斯与松嫩地块(松花江―嫩江地块)间板块俯冲碰撞或陆间洋盆消失闭合的环境。综合佳木斯地块同位素研究成果,结合该区古生物的研究和地质特点,推演出依兰地区黑龙江杂岩的形成演化模式,绘制出晚石炭世―早二叠世东北地区的岩相古地理简图。认为从晚石炭世末期开始,佳木斯地块西缘的洋壳北东向俯冲,佳木斯地块与松嫩地块沿嘉荫―牡丹江缝合带碰撞拼合,可能是在古亚洲洋南支向西伯利亚板块俯冲的大地构造背景下发生的。

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