中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Meganodular Limestone Points South China Paleoplate to the Late Ordovician Equator

文献类型:期刊论文

作者Zhan Renbin1; Jin Jisuo2; Liu Jianbo3; Zhan Renbin(詹仁斌)
刊名地质学报:英文版
出版日期2016
卷号90.0期号:1.0页码:388-389
关键词晚奥陶世 石灰石 赤道 板块 中国
ISSN号1000-9515
其他题名Meganodular Limestone Points South China Paleoplate to the Late Ordovician Equator
英文摘要Objective Time-specific litho- and biofacies often holds important information about unique ancient ecosystems that no longer exist on Earth today. This report summarizes one of such time-specific facies--the 3-D network structure of the Upper Ordovician Pagoda Formation in South China, as investigated by Zhan et al. (Palaeogeography, Palaeocli-matology, Palaeoecology, DOI: 10.1016/j.palaeo.2015.07.039).
语种中文
CSCD记录号CSCD:5626017
源URL[http://ir.nigpas.ac.cn/handle/332004/39560]  
专题中国科学院南京地质古生物研究所
作者单位1.中国科学院南京地质古生物研究所
2.Department of Earth Sciences, Western University, London Ontario
3.北京大学
推荐引用方式
GB/T 7714
Zhan Renbin,Jin Jisuo,Liu Jianbo,et al. Meganodular Limestone Points South China Paleoplate to the Late Ordovician Equator[J]. 地质学报:英文版,2016,90.0(1.0):388-389.
APA Zhan Renbin,Jin Jisuo,Liu Jianbo,&Zhan Renbin.(2016).Meganodular Limestone Points South China Paleoplate to the Late Ordovician Equator.地质学报:英文版,90.0(1.0),388-389.
MLA Zhan Renbin,et al."Meganodular Limestone Points South China Paleoplate to the Late Ordovician Equator".地质学报:英文版 90.0.1.0(2016):388-389.

入库方式: OAI收割

来源:南京地质古生物研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。