Citation: | LI Bin, CHEN Jingsheng, LIU Miao, YANG Fan, LI Wei, WU Zhen, CHEN Minhua, WU Changsheng. LA-ICP-MS zircon U-Pb geochronology and geochemical characteristics of the Early Permian granite in Chifeng area, Inner Mongolia[J]. Geological Bulletin of China, 2018, 37(9): 1671-1681. |
In this paper, the authors studied the geochronology and geochemistry of the Mingshan granitic complex and Jianshanzi granite in Chifeng area, with the purpose of providing constraints on the formation time, petrogenesis and tectonic background on the northern margin of the North China Block. The zircon U-Pb age data obtained by using laser ablation ICP-MS technique are 284.4±7.9Ma and 294.7±8.5Ma, indicating that the Mingshan granitic complex and Jianshanzi granite were formed in Early Permian. The major elements characteristics of the porphyritic biotite monzogranite are high in SiO 2 and (K2O+Na2O), with A/CNK lower than 1, belonging to high K calc-alkaline I-type granite. The syenogranite has Al2O3 14.32%~15.14%, Na2O/K2O 0.71~0.99 and A/CNK 1.17~1.20, with corundum molecule in CIPW standard mineral calculation. The porphyritic biotite monzogranite and syenogranite are similar in trace elements, with enrichment of large ion lithophile elements, loss of high-field strong elements, and obvious negative Sr, P and Ti anomalies, thus having the characteristics of island-arc magma. In combination with the geochemistry and regional geological characteristics, it is suggested that the Early Permian granites in Chifeng area was generated in an island-arc/active continental margin tectonic setting.
[1] | 王荃, 刘雪亚, 李锦轶.中国华夏与安加拉古陆间的板块构造[M].北京:北京大学出版社, 1991:56-60. |
[2] | 徐备, 陈斌.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构及演化[J].中国科学, 1997, 3:227-232. |
[3] | 徐备, 赵盼, 鲍庆中, 等.兴蒙造山带前中生代构造单元划分初探[J].岩石学报, 2014, 30(7):1841-1857. |
[4] | Xiao W J, Windley B F, Hao J, et al. Accretion leading tocollision and the Permian Solonker suture, Inner Mongolia, China:Termination of the central Asian orogenic belt[J]. Tectonics, 2003, 22:8-1. |
[5] | 张栓宏, 赵越, 刘建民, 等.华北地块北缘晚古生代-早中生代岩浆活动期次、特征及构造背景[J].岩石矿物学杂志, 2010, 29(6):824-842. doi: 10.3969/j.issn.1000-6524.2010.06.017 |
[6] | 邵济安, 何国琦, 唐克东.华北北部二叠纪陆壳演化[J].岩石学报, 2015, 31(1):47-55. |
[7] | Tang K D. Tectonic development of paleozoicfoldbelts at the north margin of the Sino-KoreanCraton[J]. Tectonics, 1990, 9(2):249-260. |
[8] | 邵济安.中朝板块北缘中段地壳演化[M].北京:北京大学出版社, 1991. |
[9] | 洪大卫, 黄怀曾, 肖宜君, 等.内蒙古中部二叠纪碱性花岗岩及其地球动力学意义[J].地质学报, 1994, (3):219-230. doi: 10.3321/j.issn:0001-5717.1994.03.001 |
[10] | Sengor A M C, Natalin B A, Burtman V S. Evolutionof the Altaid tectonic collage and paleozoiccrustalgrowth in Eurasia[J]. Nature, 1993, 364:299-307. doi: 10.1038/364299a0 |
[11] | 曹花花.华北板块北缘东段晚古生代-早中生代火成岩的年代学与地球化学研究[D].吉林大学博士学位论文, 2013. |
[12] | Zhang S H, Zhao Y, Kröner A, et al. Early Permian plutons from the northern North China Block:Constraints on continental arc evolution and convergent marginmagmatism related to the Central Asian Orogenic Belt[J]. International Journal of Earth Sciences, 2009, 98:1441-1467. |
[13] | 赵越, 陈斌, 张栓宏, 等.华北克拉通北缘及邻区前燕山期主要地质事件[J].中国地质, 2010, 37(4):900-915. doi: 10.3969/j.issn.1000-3657.2010.04.007 |
[14] | 彭斌, 王国祺, 刘乐, 等.内蒙古赤峰地区二叠纪火山岩的发现及其地质意义[J].矿物岩石地球化学通报, 2016, 35(6):1329-1340. doi: 10.3969/j.issn.1007-2802.2016.06.23 |
[15] | Liu Y S, Hu Z C, Gao S, et al. In situ, analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1):34-43. |
[16] | 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 from mantle xenoliths[J]. Journal of Petrology, 2010, 51:537-571. |
[17] | Wiedenbeck M, Allé P, Corfu F, et al. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards and Geoanalytical Research, 1995, 19(1):1-23. |
[18] | Ludwig K R. Isoplot/Ex version 3. 00: a geochronology toolkitfor microsoft excel[M]. Berkeley Geochronology Center Special Publication, California, Berkeley, 2003, 4: 1-70. |
[19] | 张旗, 王焰, 熊小林, 等.埃达克岩和花岗岩:挑战与机遇[M].北京:中国大地出版社, 2008. |
[20] | 李乘东, 张旗, 苗来成, 等.冀北中生代高Sr低Y和低Sr低Y型花岗岩:地球化学、成因及其与成矿作用的关系[J].岩石学报, 2004, 20(2):270-284. |
[21] | 黄本宏.大兴安岭地区石炭、二叠系及植物群[M].北京:地质出版社, 1993. |
[22] | 王慧, 高荣宽.内蒙古达茂旗满都拉地区早二叠世生物地层划分对比在研究[J].内蒙古地质, 1999, 2:7-20. |
[23] | 马芳, 穆治国, 刘玉琳.河北滦平球状闪长岩年代学及其地质意义[J].地质论评, 2004, 50(4):360-364. doi: 10.3321/j.issn:0371-5736.2004.04.004 |
[24] | 王惠初, 赵凤清, 李惠民, 等.冀北闪长质岩石的锆石SHRIMP U-Pb年龄:晚古生代岩浆弧的地质记录[J].岩石学报, 2007, 23(3):597-604. |
[25] | 张拴宏, 赵越, 宋彪, 等.冀北隆化早前寒武纪高级变质区内的晚古生代片麻状闪长岩——锆石SHRIMP U-Pb年龄及其构造意义[J].岩石学报, 2004, 20(3):621-626. |
[26] | Zhang S H, Zhao Y, Song B, et al. Carboniferous granitic plutons from the northern margin of the North China block:implications for a late Paleozoic active continental margin[J]. Journal of the Geological Society, 2007, 164(2):451-463. doi: 10.1144/0016-76492005-190 |
[27] | 刘建峰, 李锦轶, 孙立新, 等.内蒙古巴林左旗九井子蛇绿岩锆石U-Pb定年:对西拉木伦河缝合带形成演化的约束[J].中国地质, 2016, 43(6):1947-1962. |
[28] | 孙德有, 吴福元, 张艳斌, 等.西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据[J].吉林大学学报(地球科学版), 2004, 34(2):174-181. |
[29] | Gorton M P, Schandl E S. From continents to island arcs:a geochemical index of tectonic setting for arc-related and within-plate felsic to intermediate volcanic rocks[J]. Canadian Mineralogist, 2000, 38(5):1065-1073. |
① | 内蒙古自治区地质调查院. 1:20 万赤峰幅区域地质调查修测项目. 2000. |
② | 内蒙古自治区地质调查院. 1:20 万五分幅区域地质调查修测项目. 2000. |
③ | 河北省区域地质矿产调查研究所. 1:5 万朝阳地幅区调报告. 1996. |
④ | 吉林大学. 内蒙古 1:25万赤峰市幅地质图. 2012. |
⑤ | 中国地质科学院地质研究所. 内蒙古 1:25万西老府幅区调修测报告. 2009. |
Simplified geological map of the study area
Field photograph and micrograph of monzogranite (a, c) and syenogranite (b, d)
Zircon CL images of monzogranite (14CH24) and syenogranite (14CH10
U-Pb concordia diagrams of zircons from monzogranite (14CH24) and syenogranite(14CH10)
SiO2-(K2O+Na2O)(a) and SiO2-K2O (b) patterns of monzogranite (14CH24) and syenogranite (14CH10)
Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace elements spidergrams (b) of monzogranite (14CH24) and syenogranite (14CH10)
(Zr+Nb+Ce+Y)-TFeO/MgO(a) and (Zr+Nb+Ce+Y)-(K2O+Na2O)/CaO(b) patterns of monzogranite (14CH24) and syenogranite (14CH10)
Ta/Yb-Th/Yb patterns of monzogranite (14CH24) and syenogranite (14CH10)
YbN-(La/Yb)N and Y-Sr/Y patterns of monzogranite (14CH24) and syenogranite (14CH10)
(Y+Nb)-Rb and Rb/30-Hf-3Ta patterns of monzogranite (14CH24) and syenogranite (14CH10)