Material composition characteristics of fine particles of eolian sand in Horqin Sandy Land and its indication to provenance

doi:10.7522/j.issn.1000-694X.2023.00109

Journal of Desert Research ›› 2024, Vol. 44 ›› Issue (3): 231-246.DOI: 10.7522/j.issn.1000-694X.2023.00109

Material composition characteristics of fine particles of eolian sand in Horqin Sandy Land and its indication to provenance

Xiaoyu Han¹(), Yunping Chi¹^,²(), Yuanyun Xie¹^,², Chunguo Kang³, Peng Wu¹, Yehui Wang¹, Lei Sun¹, Zhengyu Wei¹

^1.College of Geographic Science /, Harbin Normal University，Harbin 150025，China
^2.Key Laboratory of Geographical Environment Monitoring and Spatial Information Service in Cold Regions, Harbin Normal University，Harbin 150025，China
^3.Geography Department，Harbin Institute，Harbin 150086，China

Received:2023-09-13 Revised:2023-12-04 Online:2024-05-20 Published:2024-06-11
Contact: Yunping Chi

Abstract

Abstract:

The Horqin Sandy Land is the largest semi-fixed sandy land in northern China. Tracing its material sources is of great importance to understand the formation and evolution of deserts and reconstruct the migration paths of fragments. Therefore， the composition of fine particles （<63 μm and <11 μm） of eolian sand in the Horqin Sandy Land was analyzed by petrology， elemental geochemistry， Sr-Nd isotope， TIMA automatic mineral identification and U-Pb dating of detrite zircon. The material composition of the Horqin Sandy Land was characterized and its provenance was quantitatively constrained. The geochemical indicators show that the Horqin Sandy land has experienced low chemical weathering and fractional recycling degree. The heavy mineral assemblages are mainly ilmenite， epidote， zircon， garnet， magnetite + hematite limonite， which together with the discriminant diagram of geochemical motherrock indicate that the sediments in the Horqin Sandy Land are mainly derived from medium acid magmatic mother rocks. Further constrained by Sr-Nd isotopes， the main source areas are the southern margin of the Central Asian orogenic belt and the northern margin of the North China Craton， and a small amount of dust originates from the northern border desert of China. The U-Pb ages of detrital zircons in sandy land are mainly from Mesozoic to Late Paleozoic （200-600 Ma） and Paleoproterozoic （1 518-2 000 Ma and 2 200-2 600 Ma）. The comparison with the zircon age spectrum of the potential source area shows that the fine particles in the Horqin Sandy Land contain both near-source material from the Greater Khingan Mountains in the southern margin of the Central Asian orogenic belt by wind and river transport， and ancient bedrock from the Yanshan Mountains in the northern margin of the North China Craton by river transport. Quantitative provenance results of inverse Monte Carlo model show that the Central Asian orogenic belt contributes 53.7% and the North China Craton contributes 46.3%. The synergistic effect of wind and river explains the formation of fine particles of wind-sand in the Horqin Sandy Land.

Key words: Horqin Sandy Land, geochemistry, heavy minerals, Sr-Nd isotopes, zircon U-Pb dating, material source

CLC Number:

P532

Xiaoyu Han, Yunping Chi, Yuanyun Xie, Chunguo Kang, Peng Wu, Yehui Wang, Lei Sun, Zhengyu Wei. Material composition characteristics of fine particles of eolian sand in Horqin Sandy Land and its indication to provenance[J]. Journal of Desert Research, 2024, 44(3): 231-246.

Figures/Tables 10

Fig.1 Topographic overview of the study area

Fig.2 Thin section micrographs of clastic components of sediments in the Horqin Sandy Land

Table 1 Automatic quantitative mineral content results of TIMA of <63 μm components in Horqin Sandy Land

样品	钛铁矿	绿帘石	锆石	赤铁矿/磁铁矿	铁铝榴石	榍石	金红石	石英	独居石	磷灰石
Q1	27.06	20.96	9.72	8.64	6.09	5.91	3.07	1.16	0.13	0.13
Q2	35.36	10.16	15.49	5.14	13.01	4.01	3.03	0.66	0.22	0.06
Q4	33.52	11.20	15.22	2.75	14.03	4.48	3.50	1.50	0.33	0.10
Q5	28.87	14.84	11.51	14.92	6.45	4.34	2.60	1.11	0.39	0.12
Q7	34.83	9.89	18.68	3.88	10.03	4.08	3.16	2.93	0.37	0.05
平均值	31.928	13.41	14.124	7.066	9.922	4.564	3.072	1.472	0.288	0.092

Fig.3 Standardized pattern diagram of sediment elements in the Horqin Sandy Land

Fig.4 Sr-Nd isotopic composition of sediments from the Horqin Sandy Land

Fig.5 Illustration of clastic zircon （<63 μm） in the Horqin Sand Land

Fig.6 Illustration of chemical weathering degree discrimination in the Horqin Sandy Land

Fig.7 Discriminant diagrams for sediments recycling in the Horqin Sandy Land

Fig.8 Discriminant diagrams of source-rock nature for the sediments in the Horqin Sandy Land

Fig.9 Comparison of U-Pb age spectrum of clastic zircon in the Horqin Sandy Land and potential source area

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Material composition characteristics of fine particles of eolian sand in Horqin Sandy Land and its indication to provenance

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