王志宏,龚一鸣,纵瑞文,范若颖,宋俊俊,武慧君

• 1:中国地质调查局武汉地质调查中心
• 2:中国地质大学生物地质与环境地质国家重点实验室地球科学学院
• 3:中国科学院南京地质古生物研究所
• 4:武汉凯迪工程技术研究总院有限公司

摘要(Abstract)：

西准噶尔地区的乌兰柯顺剖面从晚泥盆世朱鲁木特组至早石炭世黑山头组地层连续,单斜出露,特别是其中跨越晚泥盆世弗拉期顶部至早石炭世杜内期底部的洪古勒楞组,宏体化石、微体化石和遗迹化石以及其他相标志丰富,岩性的三分性明显:下段为灰色—灰黄色生物碎屑灰岩;中段为紫红色—灰绿色沉凝灰岩;上段为灰绿色—灰黄色生物碎屑灰岩、钙泥质碎屑岩。该剖面是我国北方构造活动区难得的完整剖面和洪古勒楞组理想的候选层型剖面。牙形刺和其他大化石的初步研究表明,该剖面洪古勒楞组的时限为晚泥盆世末弗拉期至早石炭世早杜内期。

关键词(KeyWords)： 生物地层;牙形刺;洪古勒楞组;弗拉阶;法门阶;泥盆系;石炭系;西准噶尔;新疆

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(批准号:41290260,41472001);; 中国博士后科学基金(2017M612537)联合资助

作者(Author): 王志宏,龚一鸣,纵瑞文,范若颖,宋俊俊,武慧君

DOI: 10.19839/j.cnki.dcxzz.2018.02.006

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