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作 者:高宏[1,2] 谭强[3] 王惠[3] 李玉玺[3] 武利文[3]
机构地区:[1]中国地质大学地球科学与资源学院,北京100083 [2]内蒙古自治区国土资源厅,内蒙古呼和浩特010020 [3]内蒙古自治区地质调查院,内蒙古呼和浩特010020
出 处:《地质通报》2010年第5期723-728,共6页Geological Bulletin of China
基 金:中国地质调查局项目《内蒙古金盆地区1∶5万区域地质调查》(编号:J5.3.1)资助
摘 要:开展金盆地区1∶5万区域地质调查时,在内蒙古乌兰察布盟卓资县三道营乡黑山西坡老虎沟大青山组中首次发现了早白垩世化石:介形虫Cypridea ex gr.liaoningensis,Luanpingella sp.,Djungarica camarata,Clinocypris scolia,Rhinocypris echinta,Lycopterocypris infantilis,Darwinula contracta;叶肢介Neimongolestheria?sp.及瓣鳃类Ferganoconcha quadrata,F.jorekensis等。这套含化石的湖相地层的岩石特征、化石特征均与大青山组标准剖面不同,而与冀北大店子组的岩性组合、古生物特征均可对比。按照岩石地层单位的划分原则,这套含早白垩世化石的湖相地层不属于大青山组,应从大青山组中划分出来,代表阴山地区早白垩世早期的湖相沉积地层。金盆地区存在冀北滦平盆地的大店子组层位。During 1∶50000 scale regional geological survey carried out in Jinpen area, Early Cretaceous fossils were discovered in Inner Mongolia for the first time which distribut in Daqingshan Formation, Laohugou, west slope of Heishan, Sandaoying Town, Zuozi County, Ulanqab. Fossils include Cypridea ex gr. liaoningensis,Luanpingella sp.,Djungarica camarata,Clinocypris scolia, Rhinocypris echinta,Lycopterocypris infantilis,Darwinula contracta; Neimongolestheria? sp. Ferganoconcha quadrata and F. jorekensis etc. The lithology and fossil characteristics of this lake facies stratum are different from that of the standard Daqingshan geological section; however it is comparable with Dadianzi Formation in northern Heibei. We believed that this new set of stratum should be separated from Daqingshan Formation, because it represents the Early Cretaceous lake facies stratum of Yinshan area. There is also Dadianzi Formation strata in Jinpen area which mainly developed in Luanping basin, northern Heibei.
分 类 号:P534.53[天文地球—古生物学与地层学]
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