Citation: | NIU Wenchao, REN Bangfang, DUAN Lianfeng, XIN Houtian, ZHAO Zelin, ZHANG Guozhen, ZHANG Yong. 2020. 1∶50 000 Regional Geological Map Database of the Qinghegou Map-sheet, Inner Mongolia[J]. Geology in China, 47(S1): 77-85. doi: 10.12029/gc2020Z108 |
The 1∶50 000 regional geological map (K47E010009) of the Qinghegou Map-Sheet in Inner Mongolia, as an excellent national regional geological survey map (2018), was compiled by making full use of previous regional geological survey results. Through remote sensing, geophysical and geochemical exploration, geological survey, surveyed geological cross section, large-scale mapping and other means, an in-depth investigation was conducted on the ophiolitic mélange belt, sedimentary strata, igneous rock and tectonic deformation characteristics in the region. The spatial distribution, material composition and metamorphic deformation characteristics of the ophiolitic mélange belt were identified and classified as a Carboniferous Supra-Subduction Zone (SSZ) ophiolite. A detailed analysis of igneous rocks in the area has led to the classification of three magmatic events, namely, in the Late Silurian-Devonian, Carboniferous-Early Permian and Middle Permian, and the establishment of a tectonic-magmatic evolution sequence. The strata in the area have a comprehensive stratigraphic column established and are divided into two stratigraphic subregions separated by the Baiheshan ophiolitic mélange belt with distinct differences in rock combination and sedimentary environment. The map database contains geochemical analysis data of 67 samples and zircon U–Pb dating data of 17 samples. It represents the comprehensive results of the regional geological survey of the Qinghegou Map-Sheet, which is composed of the main maps, along with the map appearance and map border, covering the attributes of sedimentary and igneous rocks, ophiolitic mélanges and other geobodies in the area. It fully reflects the structure of the orogenic belt and the geological evolution process in the area, providing basic data support for geological prospecting and in-depth investigations on orogenic belts in the Beishan area.
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[1] | He Zhenyu, Zong Keqing, Jiang Hongying, Xiang Hua, Zhang Zeming. 2014. Early Paleozoic tectonic evolution of the southern Beishan orogenic collage: insights from the granitoids[J]. Acta Petrologica Sinica, 30: 2324−2338 (in Chinese with English abstract). |
[2] | Li Xiangmin, Yu Jiyuan, Wang Guoqiang, Wu Peng. 2012. Geochronology of Jijitaizi ophiolite of Beishan aea,Gansu Provice,and its geological significance[J]. Geological Bulletin of China, 31(12): 2025−2031 (in Chinese with English abstract). |
[3] | Niu Wenchao, Duan Lianfeng, Zhao Zelin, Xin Houtian, Ren Bangfang. 2020. 1∶50 000 Regional Geological Map Database of the Qinghegou Map-sSheet, Inner Mongolia[DB/OL]. Geoscientific Data & Discovery Publishing System. (2020-06-30). DOI: 10.35080/data.A.2020.P8. |
[4] | Niu Wenchao, Ren Bangfang Ren Yunwei, Sun Lixin, Duan Xiaolong, Duan Lianfeng, Li Min, Zhang Jiahui. 2017. Discovery of Neoproterozoic Gneissic Granite from the Beishan area, Inner Mongolia: Zircon U−Pb Chronologic Evidence[J]. Geology in China, 44(2): 409−410 (in Chinese with English abstract). |
[5] | Niu Wenchao, Xin Houtian, Duan Lianfeng, Wang Genhou, Zhao Zelin, Zhang Guozhen, Zheng Yilong. 2019. The identification and subduction polarity of the Baiheshan ophiolite mélanges belt in the Beishan area, Inner Mongolia—New understanding based on the geological map of Qinghegou Sheet (1∶50 000)[J]. Geology in China, 46(5): 977−994 (in Chinese with English abstract). |
[6] | Wang Guoqiang, Li Xiangmin, Xu Xueyi, Yu Jiyuan, Wu Peng. 2014. Ziron U−Pb chronological study of the Hongshishan ophiolite in the Beishan area and their tectonic significance[J]. Acta Petrologica Sinica, 30(6): 1685−1694 (in Chinese with English abstract). |
[7] | Xiao W J, Mao Q G, Windley B F, Han C M, Qu J F, Zhang J E, Ao S J, Guo Q Q, Cleven N R, Lin S F, Shan Y H, Li J L. 2010. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 310: 1553−1594. doi: 10.2475/10.2010.12 |
[8] | Xiao W J, Ao S J, Yang L, Han C M, Wan B, Zhang J E, Zhan Z Y, Li R, Chen Z Y, Song S H. 2017. Anatomy of composition and nature of plate convergence: Insights for alternative thoughts for terminal India-Eurasia collision[J]. Science China (Earth Sciences), 60: 1015−1039. doi: 10.1007/s11430-016-9043-3 |
[9] | Yang Fulin, Zhao Zhixiong, Jia Wenyan, Yang liang, Xu Hai, Jia Yuanqin, Gao Yong. 2016. Discussion on the forming age of the Beishan group in the Beishan area, Inner Mongolia[J]. Geological Survey and Research, 39(2): 89−94 (in Chinese with English abstract). |
[10] | Yu J Y, Guo L, Li J X, Li Y G, Smithies R H, Wingate M T D, Meng Y, Chen S F. 2016. The petrogenesis of sodic granites in the Niujuanzi area and constraints on the Paleozoic tectonic evolution of the Beishan region, NW China[J]. Lithos, 256–257: 250−268. |
[11] | Zhang Jinlong, Chen Chao, Pan Zhilong, Zhang Guifeng, Zhang Huan, Li Qingji. 2017. Affirm of the Erduanjing formation and analysis of its depositional environment in Xilintaole area, Inner Mongolia[J]. Geological Survey and Research, 40(4): 274−280 (in Chinese with English abstract). |
Geotectonic location of the Beishan orogenic belt (modified from Xiao WJ et al., 2010)
Schematic diagram of 1∶50 000 regional geological map database of the Qinghegou map-sheet, Inner Mongolia