IGGCAS OpenIR  > 岩石圈演化国家重点实验室
Was there an exchange of detritus between the northern and southern Black Sea terranes in the Mesozoic-early Cenozoic
Liu, Ze1,7; Zhu, Di-Cheng1,7,8; Wang, Qing1,7; Cawood, Peter A.2,3; Ma, An-Lin4; Eyuboglu, Yener5; Wu, Fu-Yuan6; Zhao, Zhi-Dan1,7
2022-04-01
Source PublicationGONDWANA RESEARCH
ISSN1342-937X
Volume104Pages:154-171
AbstractResolving the time of rifting of the Black Sea basin is critical to reconstructing the tectonic evolution of the Pontides arc in northern Turkey. U-Pb geochronology of detrital zircons from Middle Jurassic, Upper Cretaceous, and lower Eocene formations in the Eastern Pontides (NE Turkey), as well as published data from circum-Black Sea terranes, reveals that sediments preserved along with the northern (East European Craton-Scythian Platform) and southern (Eastern and Central Pontides-southern flank of the Greater Caucasus-Transcaucasus) margins of the Eastern Black Sea basin display distinct detrital provenances. The U-Pb detrital zircon ages of the sedimentary samples from the Eastern Pontides have distinct populations with ages of -650-540, -200, -170, -80, and -50 Ma. In contrast, the ages of the sedimentary samples from the northern Black Sea terranes are characterized by age peaks of -1400 and -1100 Ma compared to those of the Eastern Pontides. Only a few detrital zircons in the range of -650-540 Ma and <200 Ma are identified in the sedimentary samples from the northern Black Sea terranes. This contrast in detrital zircon ages, together with modal analysis of the samples and published paleocurrent data, suggests that Middle Jurassic-lower Eocene sedimentary samples in the Eastern Pontides were locally sourced from Gondwana affinity crustal basement rocks and associated Mesozoic-Cenozoic igneous rocks. Furthermore, there was no exchange of detritus across the Eastern Black Sea basin during the Middle Jurassic-early Eocene. These inferences require the Eastern Black Sea basin to have rifted in a back-arc setting behind the Eastern Pontides arc by the Middle Jurassic or survived as a relict basin of the Paleotethys. Crown Copyright (c) 2021 Published by Elsevier B.V. on behalf of International Association for Gondwana Research. All rights reserved.
KeywordDetrital zircon Age spectrum Detritus exchange Eastern Pontides Eastern Black Sea basin
DOI10.1016/j.gr.2021.06.011
Funding OrganizationSecond Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program
WOS KeywordNE TURKEY IMPLICATIONS ; PONTIDES OROGENIC BELT ; PB ZIRCON CHRONOLOGY ; WHOLE-ROCK GEOCHEMISTRY ; MASSIF EASTERN PONTIDES ; LOWER CRUSTAL SOURCES ; BASEMENT NW TURKEY ; SAKARYA ZONE ; GEODYNAMIC EVOLUTION ; MAGMATIC RESPONSE
Language英语
Funding ProjectSecond Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0702] ; Chinese National Natural Science Foundation[91755207] ; Chinese National Natural Science Foundation[41225006] ; MOST of China[2016YFC0600304] ; MOST of China[2016YFC0600407] ; 111 project[B18048] ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences)[MSFGPMR201802] ; Australian Research Council[FL160100168] ; International Postdoctoral Exchange Fellowship Program[2020028]
Funding OrganizationSecond Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Chinese National Natural Science Foundation ; Chinese National Natural Science Foundation ; MOST of China ; MOST of China ; 111 project ; 111 project ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences) ; Australian Research Council ; Australian Research Council ; International Postdoctoral Exchange Fellowship Program ; International Postdoctoral Exchange Fellowship Program
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000804188500001
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/106047
Collection岩石圈演化国家重点实验室
Corresponding AuthorZhu, Di-Cheng
Affiliation1.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
2.Monash Univ, Sch Earth Atmosphere & Environm, Melbourne, Vic 3800, Australia
3.Univ St Andrews, Dept Earth Sci, North St, St Andrews KY16 9AL, Scotland
4.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Sichuan, Peoples R China
5.Karadeniz Tech Univ, Dept Geol, TR-61080 Trabzon, Turkey
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
7.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
8.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, 29 Xue Yuan Rd, Beijing 100083, Peoples R China
Recommended Citation
GB/T 7714
Liu, Ze,Zhu, Di-Cheng,Wang, Qing,et al. Was there an exchange of detritus between the northern and southern Black Sea terranes in the Mesozoic-early Cenozoic[J]. GONDWANA RESEARCH,2022,104:154-171.
APA Liu, Ze.,Zhu, Di-Cheng.,Wang, Qing.,Cawood, Peter A..,Ma, An-Lin.,...&Zhao, Zhi-Dan.(2022).Was there an exchange of detritus between the northern and southern Black Sea terranes in the Mesozoic-early Cenozoic.GONDWANA RESEARCH,104,154-171.
MLA Liu, Ze,et al."Was there an exchange of detritus between the northern and southern Black Sea terranes in the Mesozoic-early Cenozoic".GONDWANA RESEARCH 104(2022):154-171.
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