中国白垩纪综合地层和时间框架
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摘要
中国白垩系分布广泛,类型多样,以陆相地层发育为特色,海相及海陆交互相地层分布相对局限.本文对中国白垩纪地层进行了总结,完成综合地层划分与对比,为中国白垩纪研究提供时间框架.海相或海陆交互相沉积主要分布于西藏南部、喀喇昆仑、塔里木盆地西部、黑龙江东部及台湾东部,以藏南分布最为完整,浮游有孔虫化石带和菊石序列可直接与国际标准对比.陆相沉积在中西部以河湖相红色碎屑岩为主,在东部火山活动带常呈碎屑岩与中酸性火山岩共生,以冀北-辽西地区和松辽盆地发育最为完整.基于多重地层学理论,在不同区地层对比的基础上,以藏南和冀北-辽西、松辽盆地为标准,完成了海相和陆相地层的综合划分与对比,建立了中国白垩纪综合地层和时间框架.中国白垩系研究的发展将以陆相为特色,通过生物地层、同位素年龄、古地磁和旋回地层等多重划分与对比,相互验证,达到陆相与海相地层的精准对比,为白垩纪地质事件研究和矿产资源勘查等提供可依靠的时间框架.
引文
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