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四川峨眉山地质遗迹及其地学意义

DOI: 10.11867/j.issn.1001-8166.2015.06.0691, PP. 691-699

Keywords: 峨眉山,地质遗迹,地学意义,地质构造

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Abstract:

峨眉山在1996年与乐山大佛一同被列入世界自然与文化遗产名录,是自然和文化的双重遗产之地。其地质遗产以麦地坪震旦—寒武系国际层型参考剖面等典型地层剖面、新构造运动产生的峨眉山断块山等现代地貌以及独特的峨眉山玄武岩和峨眉山花岗岩为代表。以峨眉山风景区地质遗迹景观为基础,以上扬子地层分区的部分地层区域、四川盆地东缘断块山地貌单元为研究视角,构建峨眉山地质遗迹资源体系——包括5个大类、18个亚类共60余处地质遗迹景点;在峨眉山地质构造特征分析的基础上,对前人研究进行了总结,探讨了峨眉山风景区地质构造特征、地质遗迹资源体系类型与分布,以及地质遗迹的地学意义。研究表明,峨眉山风景区完整地层序列的出露是地质剖面类地质遗迹景观、古生物活动遗迹景观以及岩溶地貌景观的物质条件,新生代以来的强烈构造运动为构造地貌景观、水体景观等提供了外动力条件。峨眉山的地质遗迹研究在古生物与地层学、沉积学、地球深部动力学、构造学等方面具有重要科学意义。

References

[1]  Zhang Lei, Zhang Xujiao, Wu Fadong,et al. Characteristics and genesis of landscapes in Wangmangling National Geopark, Shanxi Province [J]. Acta Geoscientica Sinica, 2014 35(3): 383-390.[张蕾, 张绪教, 武法东, 等. 山西王莽岭国家地质公园地貌景观特征及其成因研究[J]. 地球学报, 2014,35(3): 383-390.]
[2]  Zhang Chengyu. Geological heritages functions and their relationship from the view of the world heritage [J]. Acta Scicentiarum Naturalum Universitis Pekinesis, 2006,42(2):43-47.[张成渝. 世界遗产视野下的地质遗产的功能及其关系研究[J]. 北京大学学报 :自然科学版, 2006, 42(2): 43-47.]
[3]  Bureau of Geology and Mineral Resources of Sichuan Province. Geological Map of Emei in Scale of 1∶200000[Z]. Chengdu: Bureau of Geology and Mineral Resources of Sichuan Province, 1971.[四川省地质矿产局.峨眉幅H-48-20 1/20 万地质图[Z]. 成都: 四川省地质矿产局,1971.]
[4]  Chen Meng’e. The new knowledge of the fossil assemblages from maidiping section, Emei County, Sichuan with reference to the sinian-Cambrian boundary[J]. Chinese Journal of Geology, 1982, (3): 253-262.[陈孟莪. 四川峨眉麦地坪剖面震旦系—寒武系界线的新认识及有关化石群的记述[J]. 地质科学,1982, (3): 253-262.]
[5]  Xu Daoyi, Mao Xueying, Zhang Qinwen, et al. Studies of the maidiping simian-cambrian boundary section, E’Mei County, Sichuan Province, based on the neutron activation analysis [J]. Geological Review, 1995, 41(1):74-81.[徐道一,毛雪瑛,张勤文,等. 四川峨眉麦地坪震旦系—寒武系界线剖面的中子活化分析研究[J]. 地质论评,1995, 41(1):74-81.]
[6]  Yang Xianhe, Chen Yuande, Li Shanji, et al. Division and correlation on the boundary between the precambrian and cambrian of maidiping section in Emei County Sichuan Province[C]//Bulletin Tianjin Institute Geology Mine Research, 1981.[杨暹和, 陈远德, 李善姬, 等. 四川峨眉麦地坪剖面前寒武系和寒武系界线的划分与对比[C]//中国地质科学院天津地质矿产研究所文集, 1981.]
[7]  Yue Zhao. The Discovery of Tannuolina and Lapworthella from Lower Cambrian in Meishucun (Yuannan) and Maidiping (Sichuan) sections[C]//Professional Papers of Stratigraphy and Palaoeontology (16th),1986:8.[岳昭. Tannuolina和Lapworthella在云南晋宁梅树村和四川峨山眉麦地坪剖面中发现[C]//地层古生物论文集(第十六辑),1986:8.]
[8]  Chen Shasha, Sun Keqin. Study on sustainable development of world cultural and natural heritage—A case of Mountain Emei Scenic area, including Leshan Giant Buddha Scenic area [J]. Resource Development & Market, 2010,(12): 1 141-1 143.[陈沙沙, 孙克勤. 中国世界文化—自然遗产可持续发展研究——以峨眉山—乐山大佛为例[J]. 资源开发与市场, 2010, (12): 1 141-1 143.]
[9]  Wang Yunsheng,Wang Dengpan,Wang Jiangzhen, et al. Study on the formation of the Emei faulty bock mountain[J]. South-to-North Water Transfers and Water Science & Technology, 2013,11(1):111-113,121.[王运生, 王登攀, 王奖臻, 等. 峨眉断块山的形成[J]. 南水北调与水利科技, 2013,11(1):111-113,121.]
[10]  Wan Tianfeng, Zhu Hong. Position and kinematics of Chinese continental blocks in reconstruction of global paleo-continents for Paleozoic and Triassic[J]. Geoscience, 2007, 21(1): 1-13.[万天丰, 朱鸿. 古生代与三叠纪中国各陆块在全球古大陆再造中的位置与运动学特征[J]. 现代地质, 2007, 21(1): 1-13.]
[11]  Mattauer M, Matte P, Malavieille J, et al. Tectonics of the Qinling belt: Build-up and evolution of eastern Asia[J]. Nature, 1985, 317(6 037): 496-500.
[12]  Zhao X, Coe R S. Palaeomagnetic constraints on the collision and rotation of North and South China[J]. Nature, 1987, 327(6 118): 141-144.
[13]  Yin A, Nie S. An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems, eastern Asia[J]. Tectonics, 1993, 12(4): 801-813.
[14]  Pan Jiang. World Culture and Nature Heritage of China[M].Beijing: Geological Publishing House, 2002.[潘江. 中国的世界自然遗产的地质地貌特征[M].北京:地质出版社,2002.]
[15]  Zhao Ting, Zhao Xun. Geo-heritage taxonomy and its application[J]. Acta Geoscientica Sinica, 2009,30(3): 301-308.[赵汀, 赵逊. 地质遗迹分类学及其应用[J]. 地球学报, 2009,30(3): 301-308.]
[16]  Xu Tao, Sun Hongyan, Tian Mingzhong. A discussion on the concept and taxonomic hierarchies of geological heritages[J]. Acta Geoscientica Sinica, 2011, 32(2): 211-216.[许涛, 孙洪燕, 田明中.地质遗产的概念及其分类体系[J].地球学报,2011,32(2): 211-216.]
[17]  Luo Pei, Qin Zihan, Sun Chuanmin. The geological heritage resources system of Huayingshan grand canyon geo-park in Sichuan and its geographic significance[J]. Acta Geoscientica Sinica, 2013,34(6): 738-748.[罗培, 秦子晗, 孙传敏. 四川邻水华蓥山大峡谷地质公园地质遗迹资源体系及地学意义[J]. 地球学报, 2013,34(6): 738-748.]
[18]  Huang Yunfei, Tong Jinnan. Advance in the study of the Permian-triassic bivalves [J]. Advances in Earth Science,2014,29(8):922-933.[黄云飞,童金南.古—中生代之交双壳类演变研究进展[J]. 地球科学进展, 2014,29(8):922-933.]
[19]  Chung S L, Jahn B. Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary[J]. Geology, 1995, 23(10): 889-892.
[20]  Ali J R, Fitton J G, Herzberg C. Emeishan large igneous province (SW China) and the mantle-plume up-doming hypothesis[J]. Journal of the Geological Society, 2010, 167(5): 953-959.
[21]  Xu Yigang, Zhong Sunlin. The Emeishan large igneous province: Evidence for mantle plume activity and melting conditions[J]. Geochimica, 2001, 30(1): 1-9.[徐义刚, 钟孙霖. 峨眉山大火成岩省: 地幔柱活动的证据及其熔融条件[J].地球化学, 2001, 30(1): 1-9.]
[22]  Loper D E, McCartney K. Mantle plumes and the periodicity of magnetic field reversals[J]. Geophysical Research Letters, 1986, 13(13): 1 525-1 528.
[23]  Lu Yuanfa, Huang Huiqiong, Ye Zhiliang. Chemical stratigraphy and sedimentary geochemistry of middle and lower series of Triassic in Longmendong, Emei, Sichuan[C]//Bulletin of the Chengdu Institute of Geology and Mineral Resources, the Chinese Academy of Geological Sciences,1986: 95-108.[陆元法,黄慧琼,叶志良. 峨眉龙门洞中下三叠统的化学地层和沉积地球化学[C]//中国地质科学院成都地质矿产研究所文集,1986:95-108.]
[24]  Zhang Guocheng. Wang Kun. Ichnofabrics and their sedimentary significance of the member 1 of Lower Triassic Jialingjiang Formation at Longmendong, Emei Mountains, Sichuan Province[J]. Journal of Palaeogeography, 2010,(3):281-290.[张国成,王昆. 四川峨眉山龙门洞下三叠统嘉陵江组一段遗迹组构及其沉积学意义[J]. 古地理学报,2010,(3):281-290.]
[25]  Xiao Chuantao,Gong Li, Liang Wenjun. Research on paleoecology of middle Permian-middle Triassic in the western Sichuan Basin [J]. Advances in Earth Science,2014,29(7):819-827.[肖传桃, 龚丽, 梁文君.川西地区中二叠统—中三叠统古生态研究[J]. 地球科学进展, 2014,29(7): 819-827.]

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