摘要
在恰布林组硅质岩砾石中获得较丰富的放射虫化石, 共鉴定放射虫化石13 属15 种,放射虫化石的时代为早白垩世早阿普第期, 根据地层上下关系, 将恰布林组的时代限定为早白垩世晚阿普第期。在此基础上, 结合恰布林组岩石组合特征、古水流特征、化石组合特征以及区域构造,
Abundant radiolarias are found in the gravels of conglomerates of the Qiabulin Formation. There are 13 genus and 15 species to have been identified. The age of the radiolaria is early Aptain of Cretaceous, and the one of the Qiabulin Formation is late Aptian in reference to overlying strata. The provenance of the Qiabulin Formation is volcanic arc and ophiolite complex formed in Cretaceous in the north of the Qiabulin Formation based on the sedimentary characteristics, directions of paleocurrent, fossil assemblages and regional geology.\;
出处
《现代地质》
CAS
CSCD
北大核心
1999年第3期281-286,T001,共7页
Geoscience
基金
国家自然科学基金
国家重点基础研究发展规划项目
关键词
恰布林组
放射虫
早阿普第期
早白垩世
地层
the Qiabulin Formation, radiolaria, early Aptian, late Aptian, volcanic arc, ophiolite complex