中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Ordovician geology and stratigraphy of China: A synthesis

文献类型:期刊论文

作者Zhang, Yuandong1,2,4; Zhan, Renbin1,2,4; Zhen, Yongyi3; Wang, Wenhui5; Liang, Yan1,2; Fang, Xiang1,2; Wu, Rongchang1,2; Yan, Kui1,2; Zhang, Junpeng1,2; Li, Wenjie1,2
刊名ESTONIAN JOURNAL OF EARTH SCIENCES
出版日期2023
卷号72期号:1页码:1
ISSN号1736-4728
关键词China integrative stratigraphy palaeontology Ordovician System tectonic orogeny biotic event
DOI10.3176/earth.2023.72
通讯作者Zhang, Yuandong(ydzhang@nigpas.ac.cn)
英文摘要China presently comprises several tectonic blocks and regions assembled over geological time and having independent histories. During the Ordovician, these blocks included South China, North China, Tarim, Qaidam, Junggar, Qiangtang-Qamdo, Lhasa and partially Himalaya, Sibumasu and Indochina, as well as the Altay-Xing'an and Songpan-Garze fold belts, which were discrete but adjacent. Twelve stratigraphic megaregions bounded by tectonic sutures or major fault zones are recognised for the Ordovician System. Some of them are further subdivided into regions according to specific lithological and biotic facies or distinct stratigraphic successions. The palaeontological features and biostratigraphic framework of these stratigraphic megaregions and regions are summarised. The unified biostratigraphic framework presented herein includes 33 graptolite and 27 conodont biozones through the Ordovician, together with supplementary biozones, communities or associations of brachiopods, trilobites, cephalopods, chitinozoans, acritarchs and radiolarians. With the constraints of integrative chronostratigraphy, biostra - tigraphy, chemostratigraphy, cyclostratigraphy and magnetostratigraphy, along with some geo-chronological data, our understanding of the temporal and spatial distribution of the Ordovician lithostratigraphic units on these major blocks has been significantly advanced. The refined integrative stratigraphic framework of the Ordovician provides a precise constraint on the major tectonic orogenies and biotic events evident in China.
WOS研究方向Geology
语种英语
出版者ESTONIAN ACAD PUBLISHERS
WOS记录号WOS:001018552000003
源URL[http://ir.nigpas.ac.cn/handle/332004/42485]  
专题中国科学院南京地质古生物研究所
通讯作者Zhang, Yuandong
作者单位1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironment, Nanjing 210008, Peoples R China
3.WB Clarke Geosci Ctr, Geol Survey New South Wales, Londonderry, NSW 2753, Australia
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.Cent South Univ, Sch Geosci & Info Phys, Key Lab Metallogen Predict Nonferrous Met & Geol E, Minist Educ, Changsha 410083, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Yuandong,Zhan, Renbin,Zhen, Yongyi,et al. Ordovician geology and stratigraphy of China: A synthesis[J]. ESTONIAN JOURNAL OF EARTH SCIENCES,2023,72(1):1.
APA Zhang, Yuandong.,Zhan, Renbin.,Zhen, Yongyi.,Wang, Wenhui.,Liang, Yan.,...&Li, Wenjie.(2023).Ordovician geology and stratigraphy of China: A synthesis.ESTONIAN JOURNAL OF EARTH SCIENCES,72(1),1.
MLA Zhang, Yuandong,et al."Ordovician geology and stratigraphy of China: A synthesis".ESTONIAN JOURNAL OF EARTH SCIENCES 72.1(2023):1.

入库方式: OAI收割

来源:南京地质古生物研究所

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