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    ZHANG Zhi-yong, ZHANG Ke-xin, YU Qing-wen, GONG Quan-sheng, LIANG Yun-hai, YAN Cheng-min, 2002. Method of 1∶250 000 Regional Geological Surveying in Orogenic Belts. Earth Science, 27(4): 377-385.
    Citation: ZHANG Zhi-yong, ZHANG Ke-xin, YU Qing-wen, GONG Quan-sheng, LIANG Yun-hai, YAN Cheng-min, 2002. Method of 1∶250 000 Regional Geological Surveying in Orogenic Belts. Earth Science, 27(4): 377-385.

    Method of 1∶250 000 Regional Geological Surveying in Orogenic Belts

    • Received Date: 2002-03-12
    • Publish Date: 2002-07-25
    • The paper suggests that the geological mapping of 1∶250 000 in orogenic area should take the energical theory and continental dynamics as its academic guide idea and the tectonic as the main line with the geological mapping method which combines multi-subjects. It concludes the rock construction and sequence (sedimentary rock province, magmatic rock province, metamorphic rock province, malange province) in the main tectonic units among different tectonic evolution stages in orogenic belts, paying attention to the structure, formation, evolution and basic tectonic characteristics of orogenic belts, especially to the three-dimensional structure in orogenic process and orogenic belts nowadays. From the practice and method studies of geological mapping in seven mapping areas of orogenic belts in west China arranged by Geological Survey Bureau of China during "Ninth-Five-Year plan", we suggest that we should use different geological methods in different rock provinces and summarize some theories and methods about typical rock provinces and textural geological mapping in orogenic belts respectively, such as non-Smith stratigraphy, depositional basins, intrusive igneous rocks, metamorphic rocks, three-dimensional structure and tectonic evolutional model of orogenic belts. The main aim of this paper is to provide some new systematic theories and methods about 1∶250 000 regional geological mapping in blank region of Qinghai-Tibet plateau among "new cycle general survey of land and resources" developed on large scale in China and improve the study of basic geological survey in new cycle general survey of land and resources.

       

    • 致谢: 秦皇岛板厂峪景区许国华先生在本研究采样过程中提供了莫大帮助, 现任职英国约克大学(The University of York) 的Michael Hofreiter教授在德国马普进化人类学研究所(Max Planck Institute for Evolutionary Anthropology) 工作期间曾为本研究的重复性实验提供了实验条件和技术支持, 在此一并表示衷心的感谢!
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