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滇东早奥陶世阿莫里坎砂岩相沉积
引用本文:李军,袁训来.滇东早奥陶世阿莫里坎砂岩相沉积[J].地层学杂志,1995,19(1):58-61,T001.
作者姓名:李军  袁训来
作者单位:中国科学院南京地质古生物所
摘    要:根据沉积特征、大化石、遗迹化石及微体化石等诸方面证据,认为滇东早奥陶世地层属于广泛分布于西南欧、北非、中东及纽芬兰东部的阿莫里坎砂岩相沉积。

关 键 词:滇东,早奥陶世,阿莫里坎砂岩相

Early Ordovician Armoricain quartzite facies from eastern Yunnan, China
Li Jun,Yuan Xunlai.Early Ordovician Armoricain quartzite facies from eastern Yunnan, China[J].Journal of Stratigraphy,1995,19(1):58-61,T001.
Authors:Li Jun  Yuan Xunlai
Abstract:The Early Ordovician rocks in East Yunnan are composed of elastic sediments: sandstones, shales, quartzites with iron manganese-rich intercalations and ripple-marks, cross-beddings. Trilobites Taihungshania, Neseuretus, graptolite Didymograptus deflexus,brachiopods Lingula and other inarticulate genera , trace fossil Cruzicna and acritarchs Striatotheca and Coryphidium are common. This suite of shallow water sediments is of Gres Armoricain factes Which is widespread in southwest Europe,North Africa, Middle East and East Newfoundland. The Gres Armoricain factes is considered to be inshore sediments at northern marginal areas of Early Ordovician Gondwana.
Keywords:eastern Yunnan  early Ordovician  Armoricain quartzite facies  
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