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辽宁东部地区桥头组微生物诱发沉积构造(MISS)的发现及意义

WU Zijie, ZHANG Deming, FAN Haibin, ZHANG Guoren,QIU Longwei, WANG Haipeng,ZHONG Mishan,GENG Shufeng, ZHENG Wei,GAO Fuliang, ZHAO Hanqing

wf（2022）

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Abstract
1 研究目的 辽宁东部地区位于华北克拉通的东北缘( Zhao Guochun et al., 2012). 该地区中元古代晚期—新元古代早期地层发育,层序保存完整且出露较好,是研究华北克拉通中、新元古界的关键地区之一.桥头组分布于辽宁东部的本溪、辽阳、丹东、大连等地区,曾被认为形成于新元古代晚期南华纪(辽宁省地质勘查院,2017).
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microbial induced sedimentary structure,late Mesoproterozoic to early Neoproterozoic,Qiaotou Formation,eastern Liaoning
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