Citation: | LIU Bing, LI Xiaojun, GUAN Qi, CHEN Ke, CHEN Guangyan, LI Weike, HU Shaobin, ZHANG Hu, YU Saiying. The age of basic intrusive and extrusive rocks in Funing area, southeast Yunnan Province[J]. Geological Bulletin of China, 2018, 37(11): 2021-2031. |
Basic rocks composed of Banwa-type intrusive rocks, Anding-type intrusive rocks and Longkang-type extrusive rocks are well outcropped in Funing area, southeast Yunnan Province, but they lacked chronological information. Based on regional geological investigation in Funing area, the authors applied LA-ICP-MS tech to determining the U-Pb age of zircons from intrusive and extrusive basic rocks. The weighted averages of 254.0±2.0Ma and 244.2±4.4Ma were obtained from Banwa-type intrusive rocks and Anding-type intrusive rocks respectively, and the weighted averages of 251.9±3.0Ma and 255.92±0.72Ma were obtained from Longkang-type extrusive rocks. Combined with field geological survey and comprehensive research, the authors hold that the age of the Anding-type intrusive rocks should be Middle Triassic, and the age of the Banwa-type intrusive rocks and the Longkang-type extrusive rocks should be Late Permian.
[1] | 尹红光, 李飞, 张雪松, 等.富宁洞哈钛铁矿[J].云南地质, 2008, 27(2):223-228. doi: 10.3969/j.issn.1004-1885.2008.02.015 |
[2] | 罗君烈.云南铂、铜镍、铬矿床的成矿模式[J].云南地质, 1995, 14(4):311-318. |
[3] | 薛步高.云南镍矿地质特征及找镍方向[J].云南地质, 2008, 27(1):1-11. |
[4] | 薛步高.云南镍矿地质特征及找矿前景[J].化工矿产地质, 2009, 31(2):76-84. doi: 10.3969/j.issn.1006-5296.2009.02.002 |
[5] | 朱晖, 周元昆, 李迅, 等.云南富宁尾洞岩体铜镍矿化特征及成矿条件[J].矿产勘查, 2010, 1(4):334-338. doi: 10.3969/j.issn.1674-7801.2010.04.003 |
[6] |
朱明波.云南省富宁县牙牌-安定夕卡岩型铁矿矿床特征及成因研究[D].昆明理工大学硕士学位论文, 2010: 1-74. |
[7] | 李亚辉, 蒋秀坤.云南富宁地区铜镍矿成矿地质条件分析[J].云南地质, 2012, 31(2):182-187. |
[8] | 邵新宏.云南富宁钛铁砂矿地质特征及开发前景[J].现代矿业, 2013, 534(10):58-59. doi: 10.3969/j.issn.1674-6082.2013.10.017 |
[9] | 黄庆, 李波, 周文龙, 等.云南富宁弄楼岩体岩相特征及成矿阶段划分[J].矿产综合利用, 2013(4):52-56. doi: 10.3969/j.issn.1000-6532.2013.04.014 |
[10] | 周文龙, 李波, 黄庆, 等.富宁基性岩区尾硐铜镍硫化物矿床矿化特征及矿床成因探讨[J].科学技术与工程, 2013, 13(20):5908-5914. doi: 10.3969/j.issn.1671-1815.2013.20.033 |
[11] | 赵红果, 闫晓波.云南富宁牙牌矽卡岩型磁铁矿矿床特征[J].云南地质, 2013, 32(1):42-44. doi: 10.3969/j.issn.1004-1885.2013.01.011 |
[12] |
周文龙.云南富宁基性-超基性岩区铜镍矿床地球化学特征研究[D].昆明理工大学硕士学位论文, 2013: 1-95. |
[13] |
黄庆.云南富宁尾洞铜镍矿矿床地质特征研究[D].昆明理工大学硕士学位论文, 2013: 1-66. |
[14] | 郑国龙.云南富宁县安定铜镍矿地质特征及矿床成因[J].云南地质, 2014, 33(4):550-554. doi: 10.3969/j.issn.1004-1885.2014.04.017 |
[15] | 罗坤, 付义琴.云南富宁定皇钛铁砂矿矿床成因[J].云南地质, 2014, 33(3):375-379. doi: 10.3969/j.issn.1004-1885.2014.03.016 |
[16] | 赵作新, 沈辉, 赵梓涵.云南富宁县牛场钛铁砂矿矿床成因及富集规律[J].云南地质, 2014, 33(4):520-525. doi: 10.3969/j.issn.1004-1885.2014.04.012 |
[17] | 熊风, 陶琰, 邓贤泽.云南富宁洞哈铁矿磁铁矿微量元素地球化学特征[J].矿物学报, 2015(增刊):172-173. |
[18] | 彭留伟.云南安定铜镍矿地质特征及矿床成因分析[J].资源信息工程, 2016, 31(1):45-46. |
[19] | 李政林, 刘希军, 时毓, 等.右江盆地南缘二叠-三叠纪基性岩研究及其与金矿的成矿关系探讨[J].矿物学报, 2015(增刊):227-228. |
[20] | 吴根耀, 吴浩若, 钟大赉, 等.滇桂交界处古特提斯的洋岛和岛弧火山岩[J].现代地质, 2000, 14(4):393-400. doi: 10.3969/j.issn.1000-8527.2000.04.002 |
[21] | Zhou M F, Zhao J H, Qi L, et al. Zircon U-Pb geochronology and elemental and Sr-Nd isotope geochemistry of Permian mafic rocks in the Funing area, SW China[J]. Contributions to Mineralogy & Petrology, 2006, 151(1):1-19. |
[22] | Fan W M, Zhang C H, Wang Y J, et al. Geochronology and geochemistry of Permian basalts in western Guangxi Province, Southwest China:Evidence for plume-lithosphere interaction[J]. Lithos, 2008, 102(1):218-236. |
[23] | Wang C Y, Zhou M F, Qi L. Chalcophile element geochemistry and petrogenesis of high-Ti and low-Ti magmas in the Permian Emeishan large igneous province, SW China[J]. Contributions to Mineralogy & Petrology, 2011, 161(2):237-254. |
[24] | Huang H, Du Y S, Yang J H, et al. Origin of Permian basalts and clastic rocks in Napo, Southwest China:Implications for the erosion and eruption of the Emeishan large igneous province[J]. Lithos, 2014, 208/209:324-338. doi: 10.1016/j.lithos.2014.09.022 |
[25] | 李政林, 刘希军, 许继峰, 等.右江盆地基性岩的地球化学演化特征及其区域构造意义[J].桂林理工大学学报, 2015, 35(4):727-735. doi: 10.3969/j.issn.1674-9057.2015.04.010 |
[26] | 陈雪峰, 刘希军, 许继峰, 等.桂西那坡基性岩地球化学:峨眉山地幔柱与古特提斯俯冲相互作用的证据[J].大地构与成矿学, 2016, 40(3):531-548. |
[27] | Liu X J, Liang Q D, Li Z L, et al. Origin of Permian extremely high Ti/Y mafic lavas and dykes from Western Guangxi, SW China:Implications for the Emeishan mantle plume magmatism[J]. Journal of Asian Earth Sciences, 2017, 141:97-111. doi: 10.1016/j.jseaes.2016.09.005 |
[28] | 江文, 向忠金, 夏文静, 等.滇东南富宁地区基性侵入岩与峨眉山地幔柱存在成因关系吗?——来自1:5万洞波幅和皈朝幅地质填图的证据[J].岩石学报, 2017, 33(10):3109-3122. |
[29] | 范蔚茗, 王岳军, 彭头平, 等.桂西晚古生代玄武岩Ar-Ar和U-Pb年代学及其对峨眉山玄武岩省喷发时代的约束[J].科学通报, 2004, 49(18):1892-1900. doi: 10.3321/j.issn:0023-074X.2004.18.013 |
[30] | 黄虎, 杨江海, 杜远生, 等.右江盆地上二叠统-中三叠统凝灰岩年龄及其地质意义[J].地球科学-中国地质大学学报, 2012, 37(1):125-138. |
[31] | 黄虎.右江盆地晚古生代-中三叠世盆地演化——来自沉积岩和火山岩地球化学特征的证据[D].中国地质大学(武汉)博士学位论文, 2013: 1-160. |
[32] | 张晓静, 肖加飞.桂西北玉凤、巴马晚二叠世辉绿岩年代学、地球化学特征及成因研究[J].矿物岩石地球化学通报, 2014, 33(2):163-176. doi: 10.3969/j.issn.1007-2802.2014.02.003 |
[33] | 熊风, 陶琰, 廖名扬, 等.云南富宁地区与矽卡岩型铁矿有关基性岩锆石U-Pb年龄及地球化学特征[J].矿床地质, 2014, 33(增刊):297-298. |
[34] | 皮桥辉, 胡瑞忠, 彭科强, 等.云南富宁者桑金矿床与基性岩年代测定——兼论滇黔桂地区卡林型金矿成矿构造背景[J].岩石学报, 2016, 32(11):3331-3342. |
[35] | Pearce N J G, Perkins W T, Westgate J A, et al. A Compilation of New and Published Major and Trace Element Data for NIST SRM 610 and NIST SRM 612 Glass Reference Materials[J]. Geostandards Newsletter, 2010, 21(1):115-144. |
[36] | Liu Y S, Hu Z C, Gao S, et al. In situ analysis of major and trace elements of an hydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1):34-43. |
[37] | Liu Y S, Gao S, Hu Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2):537-571. |
[38] | Anderson T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1):59-79. |
[39] | Ludwig K R. User's Manual for Isoplot 3.0:Geochronological Toolkit for Microsoft Excel[J]. Berkeley Geochronology Center Special Publication, 2003, 4:1-70. |
[40] | Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546. doi: 10.1007/s11434-010-3052-4 |
[41] | Belousova E, Griffin W, O'Reilly S Y, et al. Igneous zircon:trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy & Petrology, 2002, 143(5):602-622. |
[42] | 吴元保, 郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报, 2004, 49(16):1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002 |
[43] | 周剑雄, 陈振宇.电子探针下锆石阴极发光的研究[M].成都:电子科技大学出版社, 2007:1-104. |
[44] | 王行军, 王根厚, 专少鹏, 等.新疆和硕县包尔图一带花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报, 2012, 31(8):1251-1266. doi: 10.3969/j.issn.1671-2552.2012.08.005 |
① | 云南省地质局. 1: 20万富宁幅区域地质调查报告. 1978. |
② | 云南省地质调查院.云南1: 5万睦伦街等4幅区域地质矿产调查报告. 2017. |
③ | 李静, 张志斌, 熊家镛, 等.云南省成矿地质背景研究报告. |
Geological map of the study area
Cathodoluminescence images of zircons with analyzed spots and ages
U-Pb concordia diagrams of zircons