河南嵩山地区新元古界何家窑组微亮晶脉特征、成因及地质意义探讨
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摘要
在河南嵩山地区青白口系何家窑组中可识别出一个碳酸盐岩微亮晶脉集中的层位,笔者等结合微亮晶脉自身的特征、成分和伴生的地震引起的其他变形特征,以及通过显微镜和核磁共聚焦显微镜下的微相研究,认为嵩山地区板状微亮晶脉与华北块体东缘胶辽徐淮地区的泥晶脉特征一致,是由地震液化形成的产物,该层位代表了一个地震活跃期。同处华北块体南缘的豫西鲁山和陕西南部相对应的青白口系层位(洛峪口组和巡检司组)也发现了同期的地震记录。笔者认为嵩山地区微亮晶脉的出现应与华北块体南缘构造事件相关联。
This paper studies the horizon with carbonate microspar veins found in the Qingbaikou Hejiayao Formation in the Songshan area, Henan Province. The horizon represents a Neoproterozoic seismic activity period. Contemporaneous earthquake records were also found in the Luoyukou Formation, Lushan, western Henan Province and the Xunjiansi Formation in southern Shaanxi Province. According to the features and compositions of the microspar veins and other deformational features associated with earthquakes, especially micro-facies analysis with the confocal laser scanning microsystem (CLSM), the authors consider the banded microspar veins in the Songshan area to be the same as those found in the Jiaoliao and Xuhuai areas. The appearance of the microspar veins is related with tectonic events of the southern margin of the North China block.
This paper studies the horizon with carbonate microspar veins found in the Qingbaikou Hejiayao Formation in the Songshan area, Henan Province. The horizon represents a Neoproterozoic seismic activity period. Contemporaneous earthquake records were also found in the Luoyukou Formation, Lushan, western Henan Province and the Xunjiansi Formation in southern Shaanxi Province. According to the features and compositions of the microspar veins and other deformational features associated with earthquakes, especially micro-facies analysis with the confocal laser scanning microsystem (CLSM), the authors consider the banded microspar veins in the Songshan area to be the same as those found in the Jiaoliao and Xuhuai areas. The appearance of the microspar veins is related with tectonic events of the southern margin of the North China block.
引文
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杜远生,张传恒,韩欣,顾松竹,林文娇．2001．滇中中元古代昆阳群的 地震事件沉积及其地质意义．中国科学(D),31(4):283-289．
高林志,乔秀夫．1992．浑江末前寒武系丝状藻类及其地质意义．地 质论评,38(2):140-148．
高林志,尹崇玉,王自强．2002．华北地台南缘新元古代地层的新认 识．地质通报,21(3):131-136．
关保德,耿午辰,戎治权,杜慧英．1988．河南东秦岭北坡中-上元 古界．郑州:河南科学技术出版社,1-276．
吉林省地质矿产局．1989．吉林省区域地质志．北京:地质出版社,1- 698．
江苏地质矿产局．1984．江苏省及上海市区域地质志．北京:地质出版 社,1-857．
刘为付,孟祥化,葛铭,旷红伟,刘燕学．2004．徐州-淮南地区新元 古代臼齿碳酸盐岩成因探讨．地质论评,50(5):454-463．
辽宁省地质矿产局．1989．辽宁省区域地质志．北京:地质出版社,1- 858．
旷红伟,刘燕学,孟祥化,葛铭,蔡国印．2004．．吉辽地区新元古代臼 齿碳酸盐岩岩相的若干岩石学特征研究．地球学报,25(6):647 -653．
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马杏垣,索书田,闻立峰,等．1975．河南嵩山区震旦系古构造形式．地 质科学,(1):12-31．
彭阳,杨天南,乔秀夫,李典志,王国桢,杨中柱,杨小波．2001．大连上 震旦统地震灾变事件研究．地质学报,75(2):221-227．
潘国强,刘家润,孔庆友,等．2000．徐宿地区震旦纪地质事件及其成 因讨论．高校地质学报,6(4):566-575．
乔秀夫,宋天锐,高林志,彭阳,李海兵,高劢,宋彪,张巧大．1994．碳 酸盐岩振动液化地震序列．地质学报,68(1):16-34．
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乔秀夫,季强,高林志,章雨旭,高振家．1996．北中国板块东部震旦系 对比．中国区域地质,(2):135-142．
乔秀夫,高林志．1999．华北中新元古代及早古生代地震灾变事件及 与Rodinia的关系．科学通报,44(16):1753-1757．
乔秀夫,高林志,彭阳,李海兵．2001a．古郯庐带沧浪铺阶地震事件、 层序及构造意义．中国科学(D),31(11):911-918．
乔秀夫,高林志,彭阳．2001b．古郯庐带新元古界 灾变、层序、生 物．北京:地质出版社,1-128．
乔秀夫．2002a．中朝板块元古宙板内地震带与盆地格局．地学前缘,9 (3):141-149．
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