Stratiform siderites from the Mesoproterozoic Xiamaling Formation in North China: Genesis and environmental implications

doi:10.1016/j.gr.2018.01.013

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院油气资源研究重点实验室

	Stratiform siderites from the Mesoproterozoic Xiamaling Formation in North China: Genesis and environmental implications
	Tang, Dongjie 1,2; Shi, Xiaoying 1,3; Jiang, Ganging 4; Wu, Tong 3; Ma, Jianbai 3; Zhou, Xigiang 5
刊名	GONDWANA RESEARCH
	2018-06-01
卷号	58 页码:1-15
关键词	Stratiform siderites Dissimilatory iron reduction (DIR) Mesoproterozoic Xiamaling Formation North China Platform Columbia supercontinent
ISSN号	1342-937X
DOI	10.1016/j.gr.2018.01.013
文献子类	Article
英文摘要	Stratiform or layered siderites are much less common than siderite concretions in the stratigraphic record. In the middle part of the Mesoproterozoic Xiamaling Formation (ca. 1.40-1.35 Ga), layered siderites are widespread across the North China Platform. Facies analysis indicates that the Xiamaling siderites were formed in shallow water environments above the storm wave base. High Fe/Al and V/Al ratios and the lack of pyrites in siderite-bearing strata indicate ferruginous bottom-water conditions during the formation of siderites. The low thermal maturity of organic matter and clay mineral structures suggest that the layered siderites were formed at burial temperatures <= 90 degrees C. The negative delta C-13 values (-24 parts per thousand to -12 parts per thousand) of siderites and the presence of mu m-scale hematite inclusions in siderite grains suggest that dissimilatory iron reduction (DIR) during early diagenesis has played critical roles in siderite formation. The source of Fe-oxyhydroxides required for DIR could be from Fe(II) oxidation in shallow seawater above the redoxcline in response to enhanced hydrothermal activities or, alternatively, directly from continental Fe-oxide input. The positive cerium (Ce) and europium (Eu) anomalies of clay minerals in siderite-bearing strata and their positive correlation with total Fe contents (TFe2O3) seem to favor a hydrothermal origin of iron. Syndepositional hyalophane concretions, intermittent tuff layers, and remarkable enrichment of Cu and Zn in some of the siderite-hosting rocks provide further support to hydrothermally sourced iron. The enhanced hydrothermal activity for the development of stratiform siderites in the Xiamaling Formation probably related to the final breakup of the North China Craton from the Columbia supercontinent, during which active hydrothermal systems provided sufficient Fe(II) for Fe-redox recycling and formation of layered siderites. (C) 2018 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
WOS关键词	BANDED IRON FORMATIONS ; RARE-EARTH-ELEMENTS ; BILLION YEARS AGO ; COLUMBIA SUPERCONTINENT ; MARINE-SEDIMENTS ; WATER COLUMN ; FORMATION DEPOSITION ; FORMATION CARBONATES ; ANAEROBIC OXIDATION ; TIELING FORMATION
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000440265500001
资助机构	National Natural Science Foundation of China(41672336 ; National Natural Science Foundation of China(41672336 ; Fundamental Research Funds for the Central Universities(2652017050) ; Fundamental Research Funds for the Central Universities(2652017050) ; 41402024) ; 41402024) ; National Natural Science Foundation of China(41672336 ; National Natural Science Foundation of China(41672336 ; Fundamental Research Funds for the Central Universities(2652017050) ; Fundamental Research Funds for the Central Universities(2652017050) ; 41402024) ; 41402024) ; National Natural Science Foundation of China(41672336 ; National Natural Science Foundation of China(41672336 ; Fundamental Research Funds for the Central Universities(2652017050) ; Fundamental Research Funds for the Central Universities(2652017050) ; 41402024) ; 41402024) ; National Natural Science Foundation of China(41672336 ; National Natural Science Foundation of China(41672336 ; Fundamental Research Funds for the Central Universities(2652017050) ; Fundamental Research Funds for the Central Universities(2652017050) ; 41402024) ; 41402024)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/88160]
专题	地质与地球物理研究所_中国科学院油气资源研究重点实验室
通讯作者	Shi, Xiaoying
作者单位	1.China Univ Geosci Beijing, State Key Lab Biogeol & Environm Geol, Beijing 100083, Peoples R China 2.China Univ Geosci Beijing, Inst Earth Sci, Beijing 100083, Peoples R China 3.China Univ Geosci Beijing, Sch Earth Sci & Resources, Beijing 100083, Peoples R China 4.Univ Nevada, Dept Geosci, Las Vegas, NV 89154 USA 5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Tang, Dongjie,Shi, Xiaoying,Jiang, Ganging,et al. Stratiform siderites from the Mesoproterozoic Xiamaling Formation in North China: Genesis and environmental implications[J]. GONDWANA RESEARCH,2018,58:1-15.
APA	Tang, Dongjie,Shi, Xiaoying,Jiang, Ganging,Wu, Tong,Ma, Jianbai,&Zhou, Xigiang.(2018).Stratiform siderites from the Mesoproterozoic Xiamaling Formation in North China: Genesis and environmental implications.GONDWANA RESEARCH,58,1-15.
MLA	Tang, Dongjie,et al."Stratiform siderites from the Mesoproterozoic Xiamaling Formation in North China: Genesis and environmental implications".GONDWANA RESEARCH 58(2018):1-15.