额尔齐斯碰撞带东段结构与形成时代
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摘要
阿尔泰地体与萨吾尔岛弧之间的额尔齐斯碰撞带其结构与形成时代是中亚造山带构造演化研究的热点问题之一。本文报道了额尔齐斯碰撞带东段结构与形成时代的研究结果。新的结果显示:额尔齐斯碰撞带东段由4个走向NWNNW陡立的韧性变形带组成,剖面上呈扇状挤压变形的结构;这4个韧性变形带的应变类型为收缩应变与平面应变;片理带的变形从宏观到微观都表现出对称的结构,不同变形带不同地段可具变化的流动方向而表现出"奶油饼结构",其可能整体形成于共轴挤压机制;玉勒肯与老山口韧性变形带花岗闪长质糜棱岩、花岗闪长质超糜棱岩中变质重结晶锆石U-Pb定年结果显示韧性变形时间约为360Ma。这可能意味着早石炭世时卡拉先格尔地区已进入碰撞阶段,即萨吾尔岛弧与阿尔泰地体间在360Ma时已发生碰撞。
The texture and formation age of the Irtysh collision belt between the Altaid terrane and Sawuer oceanic island arc is one of the hottest topics surrounding the tectonic evolution of the Central Asian Orogenic Belt. In this contribution,we report new results of the texture and formation age of the eastern Irtysh collision belt. The results reveal the following evidence: 1) the eastern Irtysh collision belt is consisted of four NW-NNW-trend vertical ductile deformation zones with an asymmetrical fan-like texture in transverse profiles and the strain pattern of apparent constriction and plane strain; 2) the ductile foliation zones have macroscopic to microscopic symmetric structures with ‘cream-cake'style,and were possibly related to coaxial compression caused by the collision between the Altay terranee and Sawuer arc; and 3) the recrystallization zircons from the granodioritic mylonites and ultramylonite from the Yuleken and Laoshankou ductile deformation zone have a similar U-Pb ages of approximately 360 Ma. This indicates that the Sawuer island arc had been collided with the Altay terrane in the Early Carboniferous at approximately 360 Ma in the Kalaxiangar area.
The texture and formation age of the Irtysh collision belt between the Altaid terrane and Sawuer oceanic island arc is one of the hottest topics surrounding the tectonic evolution of the Central Asian Orogenic Belt. In this contribution,we report new results of the texture and formation age of the eastern Irtysh collision belt. The results reveal the following evidence: 1) the eastern Irtysh collision belt is consisted of four NW-NNW-trend vertical ductile deformation zones with an asymmetrical fan-like texture in transverse profiles and the strain pattern of apparent constriction and plane strain; 2) the ductile foliation zones have macroscopic to microscopic symmetric structures with ‘cream-cake'style,and were possibly related to coaxial compression caused by the collision between the Altay terranee and Sawuer arc; and 3) the recrystallization zircons from the granodioritic mylonites and ultramylonite from the Yuleken and Laoshankou ductile deformation zone have a similar U-Pb ages of approximately 360 Ma. This indicates that the Sawuer island arc had been collided with the Altay terrane in the Early Carboniferous at approximately 360 Ma in the Kalaxiangar area.
引文
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