TECTONIC ENVIRONMENT OF NAIJ TAL GROUP IN THE EAST KUNLUN OROGENIC BELT
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摘要: 纳赤台群是东昆仑造山带重要的岩石地层单位,对恢复早古生代地质演化历史具有重要意义,但对其形成构造环境分歧较大。在野外详细地质填图的基础上,对东昆仑造山带奥陶—志留系纳赤台群碎屑岩进行地球化学分析,以探讨东昆仑早古生代构造环境,为东昆仑早古生代构造演化研究提供地球化学证据。研究结果表明,纳赤台群形成于被动大陆边缘,而非活动大陆边缘的弧前盆地沉积,该结果与前人根据地质分析得出的结论一致。Abstract: The Naij Tal Group, an important stratigraphic unit, is of great significance to reconstruction of the geological evolution of the East Kunlun orogenic belt during the Early Paleozoic, but divergent opinions have been proposed about its tectonic environment. Based on close geological survey, a geochemical analysis has been made on the clastic rocks in the OrdovicianSilurian Naij Tal Group in East Kunlun orogenic belt, and the results demonstrate that this group was formed in passive continental margin, rather than in fore-arc basin on active continental margin. The study provides geochemical evidence for the study of early Paleozoic tectonic evolution in east Kunlun orogenic belt.
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Key words:
- lithogeochemistry /
- tectonic setting /
- Naij Tal Group /
- East Kunlun orogenic belt
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图 3 水泥厂纳赤台群砂岩构造环境微量元素判别图(图廓据文献[14])
A-大洋岛弧; B-大陆岛弧; C-主动大陆边缘; D-被动大陆边缘
Figure 3. Discrimination for tectonic setting of Naij Tal Group based on trace element composition of sandstones at a cement factory in East Kunlun Mountains
表 1 纳赤台群砂岩氧化物含量分析结果
Table 1. The oxides contents in the sandstones of the Naij Tal Group
表 2 判别函数值
Table 2. The values of discriminated function for the sandstones in Naij Tal Group
表 3 纳赤台群砂岩微量元素含量分析结果
Table 3. Contents of trace element of sandstones in Naij Tal Group
表 4 纳赤台群砂岩微量元素与构造性质的关系[16]
Table 4. The relationship between the trace element contents and ratios for sandstone and tectonics
表 5 纳赤台群砂岩稀土元素含量及特征参数
Table 5. REE contents and major parameters of the sandstones in Naij Tal Group
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[1] 许志琴, 杨经绥, 李海兵, 等.造山的高原——青藏高原地体的拼合、碰撞造山及隆升机制[M].北京:地质出版社, 2007. 1~458.XU Zhi-qin, YANG Jing-sui, LI Hai-bing, et al. Orogenic plateaux-terrane amalgamation, collision and uplift in the Qinghai-Tibet Plateau[M]. Beijng: Geological Publishing House, 2007. 1~458. [2] 李荣社, 计文化, 赵振明, 等.昆仑早古生代造山带研究进展[J].地质通报, 2007, 26(4) : 373~381. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd200704001&dbname=CJFD&dbcode=CJFQLI Rong-she, JI Wen-hua, ZHAO Zhen-ming, et al. Progress in the study of the Early Paleozoic Kunlun orogenic belt[J]. Geological Bulletin of China, 2007, 26(4) : 373~381. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd200704001&dbname=CJFD&dbcode=CJFQ [3] 张雪亭, 杨生德.青海省区域地质概论[M].北京:地质出版社, 2007. 98~108.ZHANG Xue-ting, YANG Sheng-de. The regional geology of Qinghai Province[M]. Beijng: Geological Publishing House, 2007. 98~108. [4] 潘裕生, 周伟明, 许荣华, 等.昆仑山早古生代地质特征与演化[J].中国科学(D辑), 1996, 26(4) : 302~307. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk199604002&dbname=CJFD&dbcode=CJFQPAN Yu-sheng, ZHOU Wei-ming, XU Rong-hua, et al. Geological features and evolution of Early Paleozoic in Kunlun orogenic belt[J]. Science in China (Series D), 1996, 26(4) : 302~307. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk199604002&dbname=CJFD&dbcode=CJFQ [5] 周春景, 胡道功, Barosh P J, 等.东昆仑三道湾流纹英安斑岩锆石U-Pb年龄及其地质意义[J].地质力学学报, 2010, 16(1) : 28~35. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100104&journal_id=dzlxxbZHOU Chun-jing, HU Dao-gong, Barosh P J, et al. Zircon U-Pb dating of the rhyolite-dcite porphyry in the Sandaowan of east Kunlun MTS and its geological significance[J]. Journal of Geomechanics, 2010, 16(1) : 28~35. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100104&journal_id=dzlxxb [6] 吴芳, 张绪教, 张永清, 等.东昆仑闹仓坚沟组流纹质凝灰岩锆石U-Pb年龄及其地质意义[J].地质力学学报, 2010, 16(1) : 44~50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100106&journal_id=dzlxxbWU Fang, ZHANG Xu-jiao, ZHANG Yong-qing, et al. Zircon U-Pb ages for rhyolite tuff of the Naocangjiangou Formation in the east Kulun orogenic belt and their implication[J]. Journal of Geomechanics, 2010, 16(1) : 44-50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100106&journal_id=dzlxxb [7] 高万里, 张绪教, 王志刚, 等.基于ASTER遥感图像的东昆仑造山带岩性信息提取研究[J].地质力学学报, 2010, 16(1) : 59~69. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100108&journal_id=dzlxxbGAO Wan-li, ZHANG Xu-jiao, WANG Zhi-gang, et al. ASTER remote sensing image-based lithologic information extraction of the east Kulun orogenic belt[J]. Journal of Geomechanics, 2010, 16(1) : 59~69. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100108&journal_id=dzlxxb [8] 张紫程, 张绪教, 高万里, 等.东昆仑左行韧性剪切带形成时代的锆石U-Pb年龄证据[J].地质力学学报, 2010, 16(1) : 51~58. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100107&flag=1ZHANG Zi-cheng, ZhANG Xu-jiao, GAO Wan-li, et al. Evidence of zircon U-Pb ages for the formation time of the east Kunlun left-lateral ductile shear belt[J]. Journal of Geomechanics, 2010, 16(1) : 51~58. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100107&flag=1 [9] 张耀玲, 张绪教, 胡道功, 等.东昆仑造山带纳赤台群流纹岩SHRIMP锆石U-Pb年龄[J].地质力学学报, 2010, 16(1) : 21~27, 50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100103&journal_id=dzlxxbZHANG Yao-ling, ZHANG Xu-jiao, HU Dao-gong, et al. SHRIMP-based zircon U-Pb ages for rhyolite of the Nachitai Group in the east Kulun orogenic belt[J]. Journal of Geomechanics, 2010, 16(1) : 21~27, 50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100103&journal_id=dzlxxb [10] 薛腊梅, 赵希涛, 张耀玲, 等.遥感技术在东昆仑新生代地质填图中的应用[J].地质力学学报, 2010, 16(1) : 70~77. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100109&journal_id=dzlxxbXUE La-mei, ZHAO Xi-tao, ZHANG Yao-ling, et al. Application of remote sensing technique in the east Kunlun Cenozoic geological mapping[J]. Journal of Geomechanics, 2010, 16(1) : 70~77. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100109&journal_id=dzlxxb [11] 陆露, 胡道功, 张永清, 等.昆中断裂带同构造花岗斑岩锆石U-Pb年龄及其构造意义[J].地质力学学报, 2010, 16(1) : 36~43. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100105&journal_id=dzlxxbLU Lu, HU Dao-gong, ZHANG Yong-qing, et al. Ziron U-Pb age for syntectoin granitic porphyry and its teceonic significance in the middle Kunlun fallt belt[J]. Journal of Geomechanics, 2010, 16(1) : 36~43. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100105&journal_id=dzlxxb [12] Siever R. Plate-tectonic controls on diagenesis[J]. Journal of Geology, 1979, 87(2) : 126~155. http://adsabs.harvard.edu/abs/1979JG.....87..127S [13] Bhatia M R. Plate tectonic and geochemical composition of sandstones[J]. Journal of Geology, 1983, 91(6) : 611~627. doi: 10.1086/628815 [14] Roser B P, Korsch R J. Plate tectonics and geochemical composition of sandstones: A discussion[J]. Journal of Geology, 1985, 93(1) : 81~84. doi: 10.1086/628921 [15] 赵振华.微量元素地球化学原理[M].北京:科学出版社, 1997. 125~129.ZHAO Zhen-hua. Geochemical principles of trace elements[M]. Beijing: Science Press, 1997. 125~129. [16] Bhatia M R, Crook K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary Basin[J]. Contributions to Mineralogy and Petrology, 1986, 92(2) : 181~193. doi: 10.1007/BF00375292 [17] 殷鸿福, 张克信, 陈能松, 等. 1: 25万冬给措纳湖幅(I47C001002)区域地质调查报告[M].武汉:中国地质大学出版社, 2003.YIN Hong-fu, ZHANG Ke-xin, CHEN Neng-song, et al. Regional geological report of Donggi Conag Hu Map (1: 250000)[M]. Wuhan: China University of Geosciences Press, 2003. [18] 王国灿, 张天平, 梁斌, 等.东昆仑造山带东段昆中复合蛇绿混杂岩带及"东昆中断裂带"地质涵义[J].地球科学——中国地质大学学报, 1999, 24(2) : 129~133. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqkx902.004&dbname=CJFD&dbcode=CJFQWANG Guo-can, ZHANG Tian-ping, LIANG Bin, et al. Composite ophiolitic mélange zone in central part of eastern section of eastern Kunlun orogenic zone and geological significance of "Fault belt in central part of eastern section of eastern Kunlun orogenic zone"[J]. Earth Science-Journal of China University, 1999, 24(2) : 129~133. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqkx902.004&dbname=CJFD&dbcode=CJFQ [19] 高延林, 吴向农, 左国朝. 东昆仑山清水泉蛇绿岩特征及其大地构造意义[R]. 西安: 中国地质科学院西安地质矿产研究所, 1988. 17~28.GAO Yan-lin, WU Xiang-nong, ZUO Guo-chao. The characters and tectonic significance of ophiolite first discovered in the east Kunlun area[R]. Xi'an: Xi'an Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 1988. 17~28. [20] 古风宝.东昆仑地质特征及晚元古代-中生代构造演化[J].青海地质, 1994, (4) : 4~13. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gtjl199401001&dbname=CJFD&dbcode=CJFQGU Feng-bao. Geological characteristics of east Kunlun and tectonic evolution in late Palaezoic-Mesozoic era[J]. Qinghai Geology, 1994, (4) : 4~13. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gtjl199401001&dbname=CJFD&dbcode=CJFQ [21] 姜春发, 杨经绥, 冯秉贵, 等.昆仑开合构造[M].北京:地质出版社, 1992. 1~224.JIANG Chun-fa, YANG Jing-sui, FENG Bing-gui, et al. Opening-closing tectonics of Kunlun orogenic zone[M]. Beijing: Geological Publishing House, 1992. 1~224. [22] 解玉月.昆中断裂东段不同时代蛇绿岩特征及形成环境[J].青海地质, 1998, (1) : 27~36. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gtjl199801003&dbname=CJFD&dbcode=CJFQXIE Yu-yue. Features of ophiolite with different period in the Eastern sector of middle Kunlun fault and its original environment[J]. Qinghai Geology, 1998, (1) : 27~36. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gtjl199801003&dbname=CJFD&dbcode=CJFQ