中国侏罗纪岩石地层划分和对比LITHOSTRATIGRAPHIC SUBDIVISION AND CORRELATION OF THE JURASSIC IN CHINA
黄迪颖,房亚男,李建国,李鑫
摘要(Abstract)：
中国的侏罗系以陆相地层为主,仅在西藏地区和黑龙江东北部发育海相地层,华南早侏罗世也存在较广泛的海相及海陆交互相沉积。中国侏罗系不同陆相盆地间的岩性和化石存在较大差异,长期以来争议很大,特别是同位素年代学和生物地层学的结果存在严重分歧。本文根据地层特征,结合大地构造和古地理等因素,将中国侏罗系分为5个大区,其中陆相盆地的基本规律为:西部区大型盆地侏罗纪沉积发育相对完整,东北—华北区缺失早侏罗世沉积,华南区普遍缺失晚侏罗世沉积,东南区同时缺失早侏罗世和晚侏罗世沉积。由此,根据最新同位素年代学、生物地层学研究结果,结合构造运动规律,本文提出了中国侏罗纪岩石地层在不同地区(盆地)的划分与对比方案。
关键词(KeyWords)： 岩石地层;地层分区;划分与对比;海相;陆相;侏罗系;燕山运动A幕;中国
基金项目(Foundation): 国家第二次青藏科考项目(2019QZKK0706);; 中国科学院战略性先导科技专项(XDB18000000、XDB26000000);; 科技部重点研发计划(2016YFC0600406);; 国家自然科学基金(41688103、41925008)共同资助
作者(Author): 黄迪颖,房亚男,李建国,李鑫
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