Citation: | YANG Jiyuan, ZHANG Jiahui, WANG Huichu, TIAN Hui, REN Yunwei, BAI Chundong, LI Jie, ZHU Benhong, KANG Chenkai, ZHOU Jing. 2020. 1∶50 000 Geological Map Database of the Dongliumafang Map-sheet at the Junction of Shanxi, Hebei and Inner Mongolia[J]. Geology in China, 47(S1): 146-161. doi: 10.12029/gc2020Z114 |
The Dongliumafang Map-sheet (K50E023002) is located in the Hengshan-Sanggan high-pressure granulite belt at the junction of Shanxi, Hebei and Inner Mongolia. The 1∶50 000 Geological Map Spatial Database of Dongliumafang Map-sheet was compiled in accordance with the Technical Requirement for Regional Geological Survey (1∶50 000) (DD 2019−01) newly issued by China Geological Survey and other relevant uniform standards and requirements, by using modern mapping technology for metamorphic rock area and digital mapping acquisition system. The map-sheet gave a detailed definition of the strata, magmatic rocks, metamorphism and tectonic structure in the Neoarchean-Cenozoic era in the area: four tectonic-lithostratigraphic units of the Neoarchean Sanggan Group and the Paleoproterozoic Jining Group, and 13 Mesoproterozoic-Cenozoic stratigraphic units have been established; the evolutionary series of Neoarchean-Paleoproterozoic and Mesoproterozoic-Mesozoic (metamorphic) intrusive rocks have been established; the structural deformation style of three periods of Early Precambrian, and the fracture structure in the Mesozoic-Cenozoic Indosinian, Yanshanian and Himalayan periods have been identified; two types of high-pressure basic granulites with different protolith properties have been identified, with metamorphic periods divided. The map-sheet uses special line segments and patterns to express the plastic rheological characteristics and structural deformation style of deep crustal rocks in the ancient orogenic belt, and has reconstructed the evolution process of Paleoproterozoic orogenic tectonics. The database adopts a MapGIS format and comprises 1∶50 000 geological map library, map appearance and corner maps, and contains nine data pieces of zircon U-Pb age, with a data volume of 53.8 MB. The 1∶50 000 Geological Map of Dongliumafang Map-sheet has innovated the mapping techniques for high-grade metamorphic areas as well as map expression methods, setting an example for mapping work on high-grade metamorphic rock areas.
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[1] | Geng Yuansheng, Shen Qihan, Ren Liudong. 2010. Late Neoarchean to Early Paleoproterozoic magmatic events and tectonothermal systems in the North China Craton[J]. Acta Petrologica Sinica, 26(7): 1945−1966 (in Chinese with English abstract). |
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[9] | Wan YS, Liu DY, Song B, Wu JS, Yang CH, Zhang ZQ, Geng YS. 2005. Geochemical and Nd isotopic compositions of 3. 8 Ga meta-quartz dioritic and trondhjemitic rocks from the Anshan area and their geological significance[J]. Journal of Asian Earth Science, 24: 563−575. doi: 10.1016/j.jseaes.2004.02.009 |
[10] | Wan Yusheng, Dong Chunyan, Ren Peng, Bai Wenqian, Xie Hangqiang, Liu Shujie, Xie Shiwen, Liu Dunyi. 2017. Spatial and temporal distribution, compositional characteristics and formation and evolution of Archean TTG rocks in the North China Craton: A synthesis[J]. Acta Petrologica Sinica, 33(5): 1405−1419 (in Chinese with English abstract). |
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[15] | Wei CJ, Qian JH, Zhou XW. 2014. Paleoproterozoic crustal evolution of the Hengshan-Wutai-Fuping region, North China Craton[J]. Geoscience Frontiers, 5(4): 485−497. doi: 10.1016/j.gsf.2014.02.008 |
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[21] | Zhao GC, Wilde SA, Sun M, Guo JH, Kröner A, Li SZ, Li XP, Zhang J. 2008. SHRIMP U-Pb zircon geochronology of the Huai'an Complex: Constraints on Late Archean to paleoproterozoic magmatic and metamorphic events in the trans-North China Orogen[J]. American Journal of Science, 308(3): 270−303. doi: 10.2475/03.2008.04 |
[22] | Zhao GC, Wilde SA, Guo JH, Cawood PA, Sun M, Li XP. 2010. Single Zircon Grains Record Two Paleoproterozoic Collisional Events in the North China Craton[J]. Precambrian Research, 177: 266−276. doi: 10.1016/j.precamres.2009.12.007 |
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[24] | Zhang HF, Wang HZ, Santosh M, Zhai MG. 2016. Zircon U-Pb ages of Paleoproterozoic Mafic Granulites from the Huai’an Terrane, North China Craton (NCC): Implications for Timing of Cratonization[J]. Precambrian Research, 272: 244−263. doi: 10.1016/j.precamres.2015.11.004 |
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[27] | Zhang Jiahui, Tian Hui, Wang Huichu, Shi Jianrong, Ren Yunwei, Chu Hang, Chang Qingsong, Zhong Yan, Zhang Kuo, Xiang Zhenqun. 2019a. Re-definition of the two-stage early-Precambrian meta-supracrustal rocks in the Huai'an Complex, North China Craton: Evidences from petrology and zircon U-Pb geochronology[J]. Earth Science, 44(1): 1−22 (in Chinese with English abstract). |
[28] | Zhang Jiahui, Wang Huichu, Tian Hui, Ren Yunwei, Shi Jianrong, Chang Qingsong, Xiang Zhenqun, Chu Hang, Wang Jiasong. 2019b. Geochemistry of the Neoarchean and Paleoproterozoic Al-rich metamorphic supracrustal rocks in the Huai’an complex, North China craton and its tectonic significances[J]. Acta Geologica Sinica, 93(7): 1618−1638 (in Chinese with English abstract). |
[29] | Zhang Jiahui, Wang Huichu, Tian Hui, Ren Yunwei, Chang Qingsong, Shi Jianrong, Xiang Zhenqun. 2019c. Petrogenesis of the MORB type high-pressure mafic granulite from the Huai'an complex in North China Craton and its tectonic implications[J]. Acta Petrologica Sinica, 35(11): 3506−3528 (in Chinese with English abstract). doi: 10.18654/1000-0569/2019.11.16 |
[30] | Zhang Jiahui, Wang Huichu, Tian Hui, Ren Yunwei, Yang Jiyuan. 2020. 1∶50 000 Geological Map Database of the Dongliumafang Map-sheet at the Junction of Shanxi, Hebei and Inner Mongolia[DB/OL]. Geoscientific Data & Discovery Publishing System. (2020-06-30). DOI: 10.35080/data.A.2020.P14. |
Paleoproterozoic tectonic zoning map of North China Craton (a, modified from Zhao GC et al., 2005) and early Precambrian geological diagram of the junction area between Shanxi, Hebei and Inner Mongolia (b)
Schematic diagram of 1∶50 000 geological map spatial database of Dongliumafang map-sheet at the junction of Shanxi, Hebei and Inner Mongolia