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地质学报  2004 

盐源―丽江构造带是新生代陆内造山带

, PP. 36-43

Keywords: 新生代陆内造山,欧亚―印度板块碰撞事件,远程效应,盐源―丽江构造带

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Abstract:

盐源-丽江构造带处于扬子大陆与青藏特提斯的结合部,其造山时代的确定,不仅对正确认识该区的构造性质与发展历史及指导矿产勘查有重要意义,而且有助于判定印度-欧亚板块碰撞事件对欧亚板块内部影响的广度和深度。通过系列构造-成矿测年,结合地层、构造、岩浆活动、成矿作用的综合研究,证实盐源-丽江构造带是新生代陆内造山带,而不是印支造山带。其造山作用主要发生于中-晚始新世之交的喜马拉雅期,与欧亚-印度板块碰撞触发的扬子大陆岩石圈向青藏特提斯岩石圈俯冲有关,表现为地壳多层次拆离、剪切和沉积盖层的滑脱、褶皱和推覆,属陆内造山,系印度-欧亚板块碰撞事件的一种远程效应。

References

[1]  国家地震局地质研究所,云南省地震局.1990.滇西北地区活动断裂.北京:地震出版社,20~27.
[2]  刘福田,刘建华,何建坤,等.2000.滇西特提斯造山带下扬子地块的俯冲板片.科学通报,45(1):79~84.
[3]  骆耀南.1985.中国攀枝花-西昌古裂谷带.见:张云湘主编.中国攀西裂谷文集(1).北京:地质出版社,1~25.
[4]  米切尔AHG,里丁HG.1985.沉积作用与大地构造.见:里丁HG主编.沉积环境和相.北京:科学出版社,553.
[5]  潘杏南,赵济湘,张选阳,等.1987.康滇构造与裂谷作用.重庆:重庆出版社,152~265.
[6]  四川省地质矿产局.1991.四川省区域地质志.北京:地质出版社,287~661.
[7]  吴正文.1990.对"大陆构造及成矿作用学术讨论会"的评述.地质论评,36(4):381~382.
[8]  杨铸生,贺金良,傅芳,等.1996.冕宁--盐源地区剪切带型金(银)矿床的成矿地质特征及找矿远景.见:骆耀南主编.扬子地台西南缘陆内造山带地质与矿产论文集.成都:四川科学技术出版社,161~170.
[9]  云南省地质矿产局.1995.云南岩相古地理图集.昆明:云南科技出版社,194~203.
[10]  周名魁,刘俨然.1988.西昌-滇中地区地质构造特征及地史演化.重庆:重庆出版社,103~190.
[11]  Bai Wenji, Hu Xufeng, Yang Jingsui, et al. 1993. No relationship between mountain-building and collision for plate tectonics.Geological Review, 39 ( 2 ): 111 ~ 116 (in Chinese with English abstract).
[12]  Bureau of Geology and Mineral Resources of Sichuan Province. 1991.Regional geology of Sichuan Province. Beijing: Geological Publishing House, 287~661 (in Chinese).
[13]  Burg J P, Brunel M, Gapais D, et al. 1984. Deformation of leucogranites of the Main Central sheet in southern Tibet (China).Journal of Structural Geology, 6: 535~542.
[14]  Foley S F, Venturelli G, Green D H, et al. 1987. The ultrapotassic rocks: classification, and constraints for petrogenetic models.Earth-Science Reviews, 24(2): 81~134.
[15]  Herren E. 1987. Zanskar shear zone: Northeast-southwest extension within the Himalayas (Ladakh, India). Geology, 15: 409~413.
[16]  Lacassin R, Seharer U, Leloup P H, et al. 1996. Tertiary deformation and metamorphism SE of Tibet: The folded Tigerleap déollement of NW Yunnan, China. Tectonics, 15(3): 605~622.
[17]  Lazarenkov V G. 1984. Tectonic position and formation series of young alkaline provinces of continents and oceans. Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 7:84~ 92 (in Russian).
[18]  Liu Zhaochang, Li Fanyou, Zhong Kanghui, et al. 1996. Tectonic evolution and metallogenesis on the western margin of the Yangtze platform. Chengdu: China Electronic Science University Press,165~219 (in Chinese with English abstract).
[19]  Luo Yaonan. 1985. Panzhihua-Xichang Paleo-Rift zone, China. In: Zhang Yunxiang, ed. Contributions to Panzhihua-Xichang Rift China (1). Beijing: Geological Publishing House, 1 ~ 25 (in Chinese).
[20]  Pan Guitang, Chen Zhiliang, Li Xingzhen, et al. 1997. Geologicaltectonic Evolution in the Eastern Tethys. Beijing: Geological Publishing House, 104 ~ 107 (in Chinese with English abstract).
[21]  Rowley D B. 1996. Age of initial collision between India and Asia: A review of stratigraphic data. Earth and Planetary Science Letters,145:1~13.
[22]  Searle M P, Pickering K, Cooper D J W. 1990. Restoration and evolution of the intermontane Indus molasses basin. Ladakh Himalaya. India. Tectonophysics, 174: 301 ~ 324.
[23]  Teng Jiwen. 1994. Physics and dynamics of lithosphere in the Kangdian Tectonic Zone. Beijing: Science Press, 161 ~ 179 (in Chinese).
[24]  Wu Zhengwen. 1990. A review of Symposium on Continental Tectonics and Metallization. Geological Review, 36 (4): 381 ~ 382(in Chinese).
[25]  Yang Zhusheng, He Jinliang, Fu Fang, et al. 1996. Geological feature of metallogenesis for shear zone type Au (Ag) deposits and its prospects in Mianning-Yanyuan area. In: Luo Yaonan, ed.Contributions to geology and mineral resources in intracontinental orogenic belt on southwestern margin of Yangtze platform.Chengdu: Sichuan Science and Technology Press, 161 ~ 170 (in Chinese with English abstract).
[26]  Zhou Mingkui, Liu Yanran. 1988. The geological tectonic characteristics and evolution in Xichang Mid-Yunnan region.Chongqing: Chongqing Publishing House, 103 ~ 190 (in Chinese with English abstract).
[27]  白文吉,胡旭峰,杨经绥,等.1993.山系的形成与板块构造碰撞无关.地质论评,39(2):111~116.
[28]  郭令智,施央申,卢华复,等.1992.印、藏碰撞的两种远距离构造效应.见:李清波等主编.现代地质学研究文集(上).南京:南京大学出版社,1~8.
[29]  刘肇昌,李凡友,钟康惠,等.1996.扬子地台西缘构造演化与成矿.成都:电子科技大学出版社,165~219.
[30]  骆耀南,傅德明,侯立玮,等.1996.扬子地台西南缘喜马拉雅期构造-岩浆-成矿作用.见:骆耀南主编.扬子地台西南缘陆内造山带地质与矿产论文集.成都:四川科学技术出版社,91~99.
[31]  潘桂棠,陈智梁,李兴振,等.1997.东特提斯地质构造形成演化.北京:地质出版社,104~107.
[32]  沈渭州,徐士进,王汝成,等.1996.四川盐源西范坪斑岩铜矿同位素地球化学研究.见:骆耀南主编.扬子地台西南缘陆内造山带地质与矿产论文集.成都:四川科学技术出版社,214~221.52.王成善.2003.成都理工大学"青藏高原地质科学学术研讨及青藏高原大陆动力学实验室2002年学术年会"上的发言.
[33]  滕吉文.1994.康滇构造带岩石圈物理与动力学.北京:科学出版社,161~179.
[34]  杨逢清,殷鸿福,杨恒书,等.1994.松潘甘孜地块与秦岭褶皱带、扬子地台的关系及其发展史.地质学报,68(3):208~218.
[35]  云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社,36~575.
[36]  赵永贵,钟大赉,刘建华,等.1992.地震层析地质解释原理及其在滇西深部构造研究中的应用.地质科学,27(2):105~113.
[37]  Bureau of Geology and Mineral Resources of Yunnan Province. 1990.Regional geology of Yunnan Province. Beijing: Geological Publishing House, 36~575 (in Chinese).
[38]  Bureau of Geology and Mineral Resources of Yunnan Province. 1995.Atlas of the sedimentary facies and paleogeography of Yunnan.Kunming: Yunnan Science and Technology Press, 194 ~ 203 (in Chinese).
[39]  Ding Lin, Zhong Dalai. 1999. Metamorphic characteristics and geotectonic implications of the high-pressure granulites from Namjagbarwa, Eastern Tibet. Science in China, 42 (5): 491~505.
[40]  Guo Lingzhi, Shi Yangshen, Lu Huafu, et al. 1992. Two kinds of remote structure effects resulting from the India and QinghaiTibet collision. In: Li Qingbo, et al., ed. Symposium of the researches on modern geology. Nanjing: Nanjing University Press, 1~8 (in Chinese).
[41]  Hodges K V, Parrish R, Housh T, et al. 1992. Simultaneous Miocene extension and shortening in the Himalayan orogen. Science, 258:1466~1470.
[42]  Institute of Geology of the State Seismological Bureau, Seismological Bureau of Yunnan. 1990. Active faults in the Northwest Yunnan. Beijing: Seismological Press, 20~ 27 (in Chinese).
[43]  Liu Futian, Liu Jianhua, He Jiankun, et al. 2000. The subducting plate of the Yangtze Block beneath the Tethyan Orogenic Zone,NW Yunnan. Chinese Science Bulletin, 45 (1): 79 ~ 84 (in Chinese).
[44]  Luo Yaonan, Fu Deming, Hou Liwei, et al. 1996. Himalayan tectonic-magmatic-metallogenic process in south-western margin of Yangtze platform. In: Luo Yaonan, ed. Contributions to geology and mineral resources in intracontinental orogenic belt on southwestern margin of Yangtze platform. Chengdu: Sichuan Science and Technology Press, 161 ~ 170 (in Chinese with English abstract).
[45]  Pan Xingnan, Zhao Jixiang, Zhang Xuanyang, et al. 1987. Tectonic and rifting in Kangdian region. Chongqing: Chongqing Publishing House, 152~265(in Chinese with English abstract).
[46]  Shen Weizhou, Xu Shijin, Wang Ruchen, et al. 1996. Isotopic geochemistry of porphyry copper deposit in Xifanping, Yanyuan County, Sichuan. In: Luo Yaonan, ed. Contributions to geology and mineral resources in intracontinental orogenic belt on southwestern margin of Yangtze platform. Chengdu: Sichuan Science and Technology Press, 214 ~ 221 (in Chinese with English abstract).
[47]  Vance D, Harris N. 1999. Timing of prograde metamorphism in the Zanskar Himalaya. Geology, 27 (5): 395 ~ 398.
[48]  Yang Fengqing, Yin Hongfu, Yang Hengshu, et al. 1994. The Songpan-Ganze massif: Its relationship with the Qinling fold belt Yangtze platform and development. Acta Geologic Sinica,68(3):208~218 (in Chinese with English abstract).
[49]  Zhao Yonggui, Zhong Dalai, Liu Jianhua. 1992. Fundamentals of geological interpretation for seismic tomogrography and its application to studying of west Yunnan\'s deep structure. Scientia Geological Sinica, 27 ( 2 ): 105 ~ 113 (in Chinese with English abstract).

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