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Neoproterozoic Diamictite of the Luoquan Formation from the North China Block and Their Implications
Sui, Peishan1,2,3; Sun, Weidong2,5; Han, Nan6; Wang, Lei7; Xie, Shiwen8; Huang, Zihang1,2,3; Wang, Xiaohong1,2,4; Gong, Hongmei1,2,4; Liu, Jin9; Lin, Jinyan10; Xiao, Yuanyuan1,2,4
2023-08-01
发表期刊JOURNAL OF EARTH SCIENCE
ISSN1674-487X
卷号34期号:4页码:1128-1139
通讯作者Xiao, Yuanyuan(yuanyuan.xiao@qdio.ac.cn)
摘要Glacial diamictite may provide important information on paleoenvironment and average composition of the upper continental crust (UCC). In this study, we report sedimentary facies, petrological and geochemical characteristics of Neoproterozoic diamictite from a profile of the Luoquan Formation on the southern margin of the North China Block (NCB). Upwards the sampling profile, lithostratigraphic strata vary from massive diamictite with poorly sorted carbonate gravels to laminated diamictite with small gravels of terrestrial detrital materials. Along the profile, CaO-MgO-LOI-Sr values decrease with the increase of SiO2-Al2O3-K2O contents. All these petrological and geochemical variations indicate a change from lodgement till deposition in the proximal of ice sheet to ice-rafting deposition in glacial-marine environment with less dolomite to supply their source. Together with previous studies on diamictite from other outcrops on the NCB, the deposition of Luoquan diamictite reflects that the glaciation on the NCB vanished and the ice-rafting effect weakened with glacial transgression process. In addition, significant co-variations of various elements with La and Al2O3 confirm the significant conservation of most analyzed elements during the sedimentary processes to produce diamictite.
关键词diamictite North China Craton paleoenvironment the Luoquan Formation Neoproterozoic sedimentation
DOI10.1007/s12583-021-1550-8
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[41776069] ; National Natural Science Foundation of China[41572047] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42020302] ; Taishan Scholar Program of Shandong[ts201712075] ; Aoshan Scholar Program of the Pilot National Laboratory for Marine Science and Technology (Qingdao)
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:001050332100014
出版者CHINA UNIV GEOSCIENCES, WUHAN
WOS关键词UPPER CONTINENTAL-CRUST ; IRON ISOTOPIC COMPOSITIONS ; SOUTH CHINA ; DOUSHANTUO FORMATION ; SQUANTUM TILLITE ; HENAN PROVINCE ; BOSTON BASIN ; HF ISOTOPES ; CONSTRAINTS ; GLACIATIONS
引用统计
被引频次:1[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/182856
专题海洋地质与环境重点实验室
深海极端环境与生命过程研究中心
通讯作者Xiao, Yuanyuan
作者单位1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China
5.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China
6.Changqing Oilfield Explorat & Dev Res Inst, Xian 710018, Peoples R China
7.Yanchang Oilfield Explorat & Dev Technol Res Ctr, Xian 716001, Peoples R China
8.Chinese Acad Geol Sci, Beijing SHRIMP Ctr, Inst Geol, Beijing 100037, Peoples R China
9.Chinese Acad Sci, Inst Oceanol, Publ Technol Serv Ctr, Qingdao 266071, Peoples R China
10.Northwest Univ, Dept Geol, Xian 710069, Peoples R China
第一作者单位中国科学院海洋研究所
通讯作者单位中国科学院海洋研究所
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GB/T 7714
Sui, Peishan,Sun, Weidong,Han, Nan,et al. Neoproterozoic Diamictite of the Luoquan Formation from the North China Block and Their Implications[J]. JOURNAL OF EARTH SCIENCE,2023,34(4):1128-1139.
APA Sui, Peishan.,Sun, Weidong.,Han, Nan.,Wang, Lei.,Xie, Shiwen.,...&Xiao, Yuanyuan.(2023).Neoproterozoic Diamictite of the Luoquan Formation from the North China Block and Their Implications.JOURNAL OF EARTH SCIENCE,34(4),1128-1139.
MLA Sui, Peishan,et al."Neoproterozoic Diamictite of the Luoquan Formation from the North China Block and Their Implications".JOURNAL OF EARTH SCIENCE 34.4(2023):1128-1139.
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