首页 | 本学科首页   官方微博 | 高级检索  
     检索      

新疆柯坪地区志留系柯坪塔格组的遗迹化石
引用本文:白忠凯,胡斌,齐永安,张国成.新疆柯坪地区志留系柯坪塔格组的遗迹化石[J].地质学报,2008,82(9):1161-1168.
作者姓名:白忠凯  胡斌  齐永安  张国成
作者单位:1. 中国石油大学盆地与油藏研究中心,北京,102249
2. 河南理工大学资源环境学院,河南焦作,454000
基金项目:国家重点基础研究发展计划(973计划),国家自然科学基金项目(面上项目,重点项目,重大项目)
摘    要:通过对柯坪地区剖面志留系的研究,在柯坪塔格组中已识别出遗迹化石15属20种,它们是:Asterichnus lawrencensis,Cochlichnus anguineus, Cruziana ichnosp., Cruziana qinlingensis, Cruziana rouaulti, Diplichnites bipartibilis,Gordia molassica, Helminthopsis abeli, Helminthopsis isp., Lockeia siliquaria ,Monocraterion cf. teataculatum, Palaeophycus tubularis, Planolites isp.,Planolites montanus, Planolites punctatus, Rusophycus ramellensis,?Scolicia ichnosp., Sagittichnus lincki,Spirophycus bicornis,Taenidium cameronensis。根据这些遗迹化石的组成、产状、分布规律及其围岩的沉积特征,可以划分为2种不同沉积环境条件下的遗迹组合,即(1)Helminthopsis-Gordia遗迹组合, 主要组成分子有Asterichnus, Diplichnites,Gorida, Helminthopsis, Planolites, Rusophycus,?Scolicia和Spirophycus,等,被解释形成于低能的滨外远岸浅海陆棚环境;(2)Cruziana-Rusophycus遗迹组合,常见组成分子有Cochlichnus,Cruziana, Lockeia, Palaeophycus,Rusophycus, Monocraterion,Sagittichnus,和Taenidium等,解释它们形成于滨外近岸浅海陆棚环境。

关 键 词:新疆  柯坪地区  志留系  柯坪塔格组  遗迹化石
收稿时间:2008/7/10 0:00:00
修稿时间:2008/7/10 0:00:00

Trace Fossils in Silurian Kepingtage Formation at Kalpin Area, Xijiang
baizhongkai,hubin,qiyong''an and zhangguocheng.Trace Fossils in Silurian Kepingtage Formation at Kalpin Area, Xijiang[J].Acta Geologica Sinica,2008,82(9):1161-1168.
Authors:baizhongkai  hubin  qiyong'an and zhangguocheng
Institution:China University of Petroleum-Beijing,Institute of Resources & Environment, Henan Polytechnic University,Institute of Resources & Environment, Henan Polytechnic University,Institute of Resources & Environment, Henan Polytechnic University
Abstract:Based on the study of Silurian outcrop at Kalpin area at the northwest of Tarim Basin, Xinjiang, 15 ichnogenus and 28 ichnospecies, namely, Asterichnus lawrencensis, Cochlichnus anguineus, Cruziana ichnosp., Cruziana qinlingensis, Cruziana rouaulti, Diplichnites bipartibilis,Gordia molassica, Helminthopsis abeli, Helminthopsis isp., Lockeia siliquaria, Monocraterion cf. teataculatum, Palaeophycus tubularis, Planolites isp.,Planolites montanus, Planolites punctatus, Rusophycus ramellensis,?Scolicia ichnosp., Sagittichnus lincki,Spirophycus bicornis and Taenidium cameronensis,were discovered in Kalpintage Formation. According to the composition, occurrence and distribution characteristics of these trace fossils and their country rock features, two types of ichnoassemblages under different sedimentary environments have been recognized as follows:(1) Helminthopsis-Gordia ichnoassemblage, including such common trace fossils as Asterichnus, Diplichnites,Gorida,Helminthopsis, Planolites, Rusophycus,?Scolicia and Spirophycus, generated in deep water shelf sedimentary environment far away the shore with lower energy; and (2)Cruziana-Rusophycus ichnoassemblage, containing such trace fossils as Cochlichnus, Cruziana, Palaeophycus, Lockeia, Rusophycus,Monocraterion,Sagittichnus and Taenidium, formed in shallow water shelf sedimentary environment.
Keywords:Xinjiang  Kalpin area  Silurian  Kepingtage formation  Trace fossils
本文献已被 维普 万方数据 等数据库收录!
点击此处可从《地质学报》浏览原始摘要信息
点击此处可从《地质学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号