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哀牢山―金沙江岩带透辉石花岗岩锆石SHRIMPU-Pb年龄及地质意义――以玉召块、马头湾和十里村岩体为例

, PP. 35-43

Keywords: SHRIMPU-Pb年龄,锆石,钾质碱性花岗岩,玉召块,马头湾,十里村,金平县,云南省

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Abstract:

位于哀牢山―金沙江新生代钾质碱性岩浆岩带南段的玉召块、马头湾和十里村透辉石花岗岩锆石SHRIMP定年结果为38Ma、34Ma和37Ma,相当于渐新世,属于喜马拉雅期,结合岩石化学、微量元素、稀土元素和Sr、Nd、Pb同位素组成等,对控岩机制、岩石的属性和成因以及锆石的成因进行探讨。

References

[1]  毕献武,胡瑞忠,叶造军,邵树勋. 1999 . A型花岗岩类与铜成矿关系研究.中国科学(D辑),29(6):489.
[2]  蔡新平. 1992. 扬子地台西缘新生代富碱斑岩中的深源包体及其意义. 地质科学,27(2):183-189.
[3]  邓万明,黄萱,钟大赉. 1998. 滇西新生代富碱斑岩的岩石特征与成因. 地质科学, 33(4):412-425.
[4]  费鼎. 1983. 南海北部区域构造和陆壳向洋壳转化. 地球物理学报. 26(5): 459-467.
[5]  黄智龙,刘丛强,朱成明. 1999. 云南老王寨金矿区煌斑岩成因及其与金矿化的关系. 北京:地质出版社, 1-251.
[6]  胡瑞忠,毕献武,Turner G and Burnard P G. 1997. 马厂箐铜矿床黄铁矿流体包裹体He-Ar同位素体系. 中国科学(D辑),27(6):503-508.
[7]  李献华,周汉文,韦刚健,刘颖,钟孙霖,罗清华,李寄?. 2002. 滇西新生代超钾质煌斑岩的元素和Sr-Nd同位素特征及其对岩石圈地幔组成的制约. 地球化学,31(1):26-34.
[8]  梁华英,谢应雯,张玉泉. 2004. 富钾碱性岩体形成演化对铜矿成矿制约――以马厂菁铜矿为例. 自然科学进展,14(1):116-120.
[9]  吕伯西,钱祥贵. 1999. 滇西新生代碱性火山岩、富碱斑岩深源包体岩石学研究. 云南地质, 18(2):127-143.
[10]  舒小辛. 1995. 云南马关地区碧玄岩中单辉橄榄岩包体的成因. 岩石矿物学杂志, 14(1):47-51.
[11]  宋彪,张玉海,万渝生,简平. 2002. 锆石SHRIMP 样品靶制作、年龄测定及有关现象讨论. 地质论评, 48(增刊):26-30.
[12]  王江海,尹安,Harrison T M,Grove M,周江羽,张玉泉,解广轰. 2002. 青藏东缘新生代两类高钾岩浆活动的热年代学研究. 中国科学(D辑), 32(7):529-537.
[13]  王联魁,夏斌,张玉泉,陈根文. 2003. 研究“钾质和钠质两个地幔富碱岩浆体系”的刍议. 高校地质学报,9(4) :545-555.
[14]  谢应雯,张玉泉. 1988. 云南十里村透辉石花岗岩特征及成因探讨. 地球化学, 4:301-309.
[15]  谢应雯,张玉泉. 1995. 云南洱海东部新生代岩浆岩岩石化学. 岩石学报,11(4):423-433.
[16]  谢应雯,张玉泉,钟孙霖,李献华.1999. 云南洱海东部新生代高钾碱性岩浆岩痕量元素特征. 岩石学报,15(1):75-82.
[17]  张玉泉,谢应雯,涂光炽. 1987. 哀牢山―金沙江富碱侵入岩及其与裂谷构造关系的初步研究. 岩石学报, 5(1):17-26.
[18]  张玉泉,谢应雯. 1994. 青藏高原及邻区富碱侵入岩――以苦干子和太和二岩体为例. 中国科学(B辑),24(10):1102-1108.
[19]  张玉泉,谢应雯. 1997. 哀牢山―金沙江富碱侵入岩年代学和Sr、Nd同位素组成. 中国科学(D辑),27(4): 289-293.
[20]  张玉泉,谢应雯,李献华,邱华宁,赵振华,梁华英. 2000. 青藏高原东部钾玄岩系岩浆岩同位素特征:岩石成因及其构造意义. 中国科学(D辑), 30(5):493-498.
[21]  Bi Xianwu, Hu Ruizhong, Ye Shaojun and Shao Shuxun. 1999. Study in the relation of A-type granitic magmatism and the copper mine fashion. Science in China (Series D), 29(6): 489-195.
[22]  Cai Xinpin. 1992. Discovery of deep-derived xenoliths in Cenozoic alkali-rich porphyries along the margin of the Yangtze platform and its significance. Scientia Geologica Sinica, 27(2): 183-189.
[23]  Composton W, Williams I S and Meyer C. 1984. U-Pb geochronology of zircons from lunar breccia 73217 using a sen?
[24]  魏启荣.2002.青藏东缘新生代两期高钾岩系中深源包体的岩石学和地球化学研究――以云南马关和六合地区为例(博士后出站报告).sitive high mass-resolution ion microprobe. J Geophys Res, 89: B525-534.
[25]  Cox K G, Bell J D and Pankhurst R J. 1979. The interpretation of igneous rocks. George, Allen and Unwin, London.
[26]  Dewey J F, Shackleton R M, Chang Chengfa et al. 1988. The tectonic evolution of the Tibetan plateau. Phil Trans R Soc Lond, A327, 379-413.
[27]  Fei Ding. 1983. Area structure in the north of South China Sea and the transform from continent to ocean. Acta Geophysica Sinica, 26(5): 459-467.
[28]  Wang Jianghai, Yin An, Harrison T M, Grove M, Zhou Jiangyu, Zhang Yuquan and Xie Guanghong. 2002. Studying of heat geochronology of two kinds of Cenozoic potassic-rich magma function in eastern Tibet. Science in China (Series D), 32(7): 529-537 (in Chinese).
[29]  Wang Liankui, Xia Bin, Zhang Yuquan and Chen Genwen. 2003. A humble Opinion on the “potassic and sodic two-mantle alkali-rich magma systems”. Geological Journal of China Universities, 9(4): 545-555 (in Chinese with English abstract).
[30]  Williams I S. 1992. Some observations on the use of zircon U-Pb geochronology in the study of granitc rocks. Trans R Soc Edinburgh-Earth Sci, 83: 447-458.
[31]  Williams I S. 1998. U-Th-Pb geochronology by ion microprobe. In Mckibben M A, Shanks W C and Ridley W I, eds., Applications of microanalytical techniques to understanding mineralizing processes. Review of Economic Geology, 7:1-35.
[32]  Wyllie P J and Sekine T. 1982. The formation of mantle phlogopite in subduction zone hybridization. Contrib Mineral Petrol, 79:375-380
[33]  Xie Yingwen and Zhang Yuquan. 1988. The characteristics and origin of diopside granite in Shilicun, Yunnan. Geochimica, 4: 301-309 (in Chinese with English abstract) .
[34]  Xie Yingwen and Zhang Yuquan. 1995. Petrochemistry of the Cenozoic magmatic rocks in the Eastern Erhai, Yunnan Province. Acta Petrologica Sinica, 11(4): 423-433 (in Chinese with English abstract).
[35]  Xie Yingwen, Zhang Yuquan, Zhong Sunlin and Li Xianghua. 1999. Trace element characteristics of the Cenozoic high-K alkaline magmatic rock series in the eastern Erhai, Yunnan Province. Acta Petrologica Sinica, 15(1): 75-82 (in Chinese with English abstract).
[36]  Zhang Yuquan, Xie Yingwen and Tu Guangchi. 1987. Preliminary studies of the alkali-rich intrusive rocks in the Ailaoshan-Jinshajiang belt and their bearing on rift tectonics. Acta Petrologica Sinica, 5(1): 17-26 (in Chinese English abstract).
[37]  Zhang Yuquan and Xie Yingwen. 1994. Alkaline-rich intrusive rocks in Qinghai-Xizang Plateau and its neighboring district. Science in China (Series B), 23(10): 1102-1108 (in Chinese).
[38]  Zhang Yuquan and Xie Yingwen. 1995. Geochemistry of granitoid rocks in Hengduan Mountains region. Beijing: Science Press, 48-58 (in Chinese).
[39]  Zhang Yuquan and Xie Yingwen. 1997. Geochronology of Ailaoshan-Jinshajing alkali-rich intrusive rocks and their Sr and Nd isotopic characteristics. Science in China(Series D), 26(4):289-293 (in Chinese with English abstract).
[40]  Zhang Yuquan, Xie Yingwen, Li Xianhua, Qiu Huaning, Zhao Zhenhua and Liang Huaying. 2000. Isotopic characteristics of shoshonitic rocks in eastern Qinghai-Tibet Plateau: Petrogenesis and its tectonic implication. Science in China (Series D), 30(5): 493-498 (in Chinese).
[41]  Deng Wanming, Huang Xuan and Zhong Dalai. 1998. Petrological characteristics and genesis of cenozoical kali-rich porphyry in west Yunnan. Scientia Geologica Sinica, 33(4): 412-425 (in Chinese with English abstract).
[42]  Hu Ruizhong, Bi Xianwu, Turner G and Burnard P G. 1997. The He?Ar isotopic system of inca stone’s fluid and inclusion in copper deposit, Machangjing. Science in China(Series D), 27(6):503-508.
[43]  Li Xianhua, Zhou Hanwen, Wei Gangjian, Liu Ying, Zhong Sunlin, Luo Qinghua and Li Jiyu. 2002. Geochemistry and Sr-Nd isotopes of Cenozoic ultrapotassic lamprophyres in western Yunnan: Constraints on the composition of sub-continental lithospheric mantle. Geochimica, 31(1): 26-33 (in Chinese with English abstract ).
[44]  Liang Huaying, Xie Yingwen and Zhang Yuquan. 2004. Formation and evolution of potassic-rich alkali rocks and their constraints on copper ore metallogenesis. Progresses in Natural Science, 14(1): 116-120 (in Chinese).
[45]  Lu Boxi and Qian Xianggui. 1999. The study of petrology in the alkali-volcanic rock in western Yunnan and Plutonic inclusion of the alkali-rich porphyry. Geology of Yunnan, 18(2): 127-143 (in Chinese).
[46]  Petro W L , Vogel T A and Wilband . 1979. Major-element chemistry of plutonic rock suites from compressional and extensional plate boundaries. Chem Geol, 26: 217-235.
[47]  Philippe Patriat and Jose Achache. 1984. India-Eurasia collision chronology has implications for crustal shortening and driving mechanism of plates. Nature, 311(18): 615-621.
[48]  Shu Xiaoxin. 1995. The genesis of Cpx-perdotitic Xenoliths in basanite of Maguan, Yunnan Province. Acta Petrologica et Mineralogical, 14(1): 47-51 (in Chinese with English abstract ).
[49]  Song Biao, Zhang Yuhai, Wan Yusheng and Jian Ping. 2002. Mount making and procedure of the SHRIMP dating. Geological Review, 48(Sup.): 26-30 (in Chinese with English abstract ) .
[50]  Sun S-s and McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalt: Implications for mantle composition and processes. Geol Soc Spec Pub, 42: 528-548.
[51]  Tapponnier P, Peltzer G, Le Dain A Y and Armijo R. 1982. Propogating extrusion tectonics in Asia: new insights from simple experiments with plasticine. Geology, 10: 611-616.
[52]  Tu Guangchi, Zhang Yuquan and Zhao Zhenhua. 1982. Preliminary studies on two alkali?rich intrusive belts in South China. In: Geology of granites and their metallogenetic ralations. Proceedings of the International Symposium. Held at Nanjing University, Nanjing, China, 33-54.

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