Arid
DOI10.1007/s12303-019-0008-9
Elemental geochemical characteristics of Lower-Middle Permian mudstones in Taikang Uplift, southern North China Basin: implications for the FOUR-PALEO conditions
Liang, Qingshao1,2; Tian, Jingchun1,2; Zhang, Xiang1,2; Sun, Xiao3; Yang, Chenyu4
通讯作者Tian, Jingchun
来源期刊GEOSCIENCES JOURNAL
ISSN1226-4806
EISSN1598-7477
出版年2020
卷号24期号:1页码:17-33
英文摘要The paleo-sedimentary environment can be restored qualitatively or semiqualitatively using elements or combinations of elements that are sensitive to the depositional environment. Through the analysis and testing of the main elements, trace elements and rare earth elements of twenty-one Lower-Middle Permian coal-bearing strata mudstone samples in Taikang Uplift, southern North China Basin, this study explored the FOUR-PALEO conditions (paleo-water depth, paleo-redox conditions, paleoclimate and paleo-provenance). The La and Co contents indicate that the water depth of the northern margin of the southern North China Basin became gradually shallower during the Lower-Middle Permian period. According to the U/Th, U-au, V/Cr, Ni/Co and V/Sc ratios, it is known that this section of the basin is in an oxidizing environment, and the oxidation is gradually enhanced from the Taiyuan Formation to the Lower Shihezi Formation. Paleoclimate from bivariate plot diagrams of C-value and Sr/Cu versus Ga/Rb shows that the Taikang Uplift was characterized by a warm and arid climate during the depositional period of Permian Taiyuan Formation and a warm and humid climate during the Lower Shihezi Formation and shows that the depositional period of Permian Shanxi Formation was in a transitional period of humid and arid. CIA, PIA, ICV, Th/U and K/Rb reflect the tectonic settings of the source area. From the Taiyuan Formation to the Lower Shihezi Formation, the CIA and PIA gradually increase, and the ICV gradually decreases, indicating enhanced chemical weathering and the transition from arid to humid in the source area, the arid and humid frequent change in the Taiyuan Formation, and a sudden climate change in the Shanxi Formation. Additionally, the provenance discriminant function, Zr/Sc-Th/Sr, REEs ratios, Th versus Hf-Co, Hf versus La/Th and ZREE vs. La/Yb indicate that the type of provenance is associated with magmatic differentiation. Moreover, discriminant diagrams, consisting of K2O/Na2O versus SiO2, La-Th-Sc, Th-Sc-Zr/10 and Th-Co-Zr/10, suggest that the mudstones of Lower-Middle Permian were deposited in active continental margin tectonic settings.
英文关键词geochemical characteristics paleoenvironment Lower-Middle Permian southern North China Basin
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000511879100002
WOS关键词DEPOSITIONAL ENVIRONMENT ; ORGANIC-MATTER ; BLACK SHALES ; SOURCE ROCKS ; EVOLUTION ; TRACE ; PROVENANCE ; SEDIMENTS ; AFRICA ; CONSTRAINTS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/314616
作者单位1.Chengdu Univ Technol, Inst Sedimentary Geol, 1 Dongsanlu, Chengdu 610059, Sichuan, Peoples R China;
2.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Peoples R China;
3.SINOPEC North China Co, Explorat & Dev Res Inst, Zhengzhou 450006, Peoples R China;
4.Sichuan Bur Geol & Mineral Resources, Geochem Team, Deyang 618000, Peoples R China
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GB/T 7714
Liang, Qingshao,Tian, Jingchun,Zhang, Xiang,et al. Elemental geochemical characteristics of Lower-Middle Permian mudstones in Taikang Uplift, southern North China Basin: implications for the FOUR-PALEO conditions[J],2020,24(1):17-33.
APA Liang, Qingshao,Tian, Jingchun,Zhang, Xiang,Sun, Xiao,&Yang, Chenyu.(2020).Elemental geochemical characteristics of Lower-Middle Permian mudstones in Taikang Uplift, southern North China Basin: implications for the FOUR-PALEO conditions.GEOSCIENCES JOURNAL,24(1),17-33.
MLA Liang, Qingshao,et al."Elemental geochemical characteristics of Lower-Middle Permian mudstones in Taikang Uplift, southern North China Basin: implications for the FOUR-PALEO conditions".GEOSCIENCES JOURNAL 24.1(2020):17-33.
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