首页> 中文期刊>中国科学 >Isotopic characteristics of shoshonitic rocks in eastern Qinghai-Tibet Plateau: Petrogenesis and its tectonic implication Isotopic characteristics of shoshonitic rocks in eastern Qinghai-Tibet Plateau: Petrogenesis and its tectonic implication

Isotopic characteristics of shoshonitic rocks in eastern Qinghai-Tibet Plateau: Petrogenesis and its tectonic implication Isotopic characteristics of shoshonitic rocks in eastern Qinghai-Tibet Plateau: Petrogenesis and its tectonic implication

     

摘要

[1]Ding Chaojian, Wang Zeng, Shentu Baoyong, Nd, Sr isotopic characteristics of main mineralization rock bodies for the Yulong Cu ( Mo ) ore belt in eartern Tibet, Contribution to the Geology of the Qinghai-Xizang (Tibet) Plateau (20) (in Chinese), [2]Beijing: Geological Publishing House, 1990, 226-230.[2]Zhang Yuquan, Xie Yingwen, Geochronology of Ailaoshan-Jinshajiang alkali-rich intrusive rocks and their Sr and Nd isotopic characteristics, Science in China, Ser. D, 1997, 40 (5): 522.[3]Ma Hongwen, Petrology and Mineralization of Granites in Yulong Porphyry Copper Belt (in Chinese), Tibet, Wuhan: China University of Geosciences Press, 1990, 112-119.[4]Zhang Yuquan, Xie Yingwen, Qiu Huaning et al., Shoshonitic series: Sr,Nd and Pb isotopic compositions of ore-bearing porphyry for Yulong copper ore belt in the eastern Tibet, Scientia Geological Sinica (in Chinese), 1998, 33 (3): 359.[5]Dosso, L., Murthy, V. R., A Nd isotopic study of the Kerguelen Island: Inference on riched oceanic mantle sources, Earth Planet Sci. Lett., 1980, (48): 268.[6]Lameyre, J., Marot, A., Ziminesv et al., Chronological evolution of the Kerguelen Island, syenite-granite ring complex, Nature, 1976, GB(26): 306. [7]Vollmer, R., Norry, M. J., Possible origin of K-rich volcanic rocks from Virunga, East Africa, by metasomatism of continental crustal materical: Pb Nd and Sr isotopic evidences, Earth Planet Sci. Lett., 1983, (64): 374.[8]Sun, S. S., McDonough, W. F., Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes, in Magmatism in the Ocean Basins, (eds. Saunders, A. D., Norry, M. J.), Geological Society Special Publication, 1989, 42: 313.[9]Hart, S. R., A large-scale isotope anomaly in the southern Hemisphere mantle, Nature, 1984, 309: 753.[10]Zhang Yuquan, Xie Yingwen, Liang Huaying et al., Petrogenesis series and ore-bearing porphyries of the Yulong ccopper ore belt in eastern Tibet, Geochimica(in Chinese), 1998, 27 (3): 236.[11]Muller, D., Rock, N. M. S., Groves, D. I., Geochemical discrimination between shoshonitic and potassic volcanic rocks from different tectonic setting: a pilot study, Mineral. Petrol., 1992, (46): 259.[12]Liu Huairen, Observation in East Africa Rift, Tectonic Evolution and Mineralization of the Tethys in Western China (ed. Chengdu Institute of Geological and Mineral Resources, Chinese Academy of Geological Sciences)(in Chinese), Chengdu: Electron University of Science and Technology Publishing House, 1991, 366.[13]He Yunzhong, Remote sensing geological characteristics and looking for ore deposit in Yulong porphyry copper zone, Eastern Tibet, Tibet Geology (in Chinese), 1992, (1): 22.[14]Tang Renli, Luo Huaisong, The Geology of Yulong Porphyry Cu (Mo) Ore Belt, Tibet (in Chinese), Beijing: Geological Publishing House, 1995, 1-40.[15]Yan Xianfu, Geological characteristics of certain rift basin in Yunnan Province and their apply effect for geophisic survey, Yunnan Geology(in Chinese), 1982, 1 (1): 47.[16]Fei Ding, On the structural feature and the oceanization in the north part of South China Sea , Acta Geophysical Sinica(in Chinese), 1983, 26 (5): 459.[17]Yu Wenjie, Geological features of the middle section of the joint zone in Jinsha River, Tibet Geology, 1993, (2): 26.

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