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辽宁本溪火连寨寒武系岩石学特征及沉积环境分析
AN ANALYSIS OF PETROGRAPHY AND SEDIMENTARY ENVIRONMENT OF CAMBRIAN IN HUOLIANZHAI,BENXI, LIAONING PROVINCE
【摘要】 以新发现的Dictyonemaflabelliforme-Staurograptus笔石带的典型分子和带化石,结合岩性及其组合特征确定了本溪火连寨寒武系-奥陶系的界限。在系统描述岩性的基础上对该区上寒武统沉积发展史及沉积环境进行了分析。
【Abstract】 The boundary between Cambrian and Ordovician in Huolianzhai is determined from typical meleculea and fossilsin the newly discovered Dictyonema flalelliborme-Staurograptus graptolite belts, intergrated with lithology and combina-tion features. on the basis of systematic description of lithoiogy, sedimentary history and environment of Upper Cam-brian in this area are analysed.
【关键词】 本溪火连寨;
寒武系;
奥陶系;
碳酸盐岩;
沉积环境;
【Key words】 Huolianzhai; Benxi Cambrian Ordovician Carbonatite Sedimentary environment;
【Key words】 Huolianzhai; Benxi Cambrian Ordovician Carbonatite Sedimentary environment;
- 【文献出处】 新疆石油地质 ,XINJIANG PETROLEUM GEOLOGY , 编辑部邮箱 ,1994年03期
- 【分类号】P534.41
- 【被引频次】3
- 【下载频次】196