J4

• 地质与资源 • 上一篇    下一篇

黑龙江省鸡西盆地基性岩40Ar/39Ar同位素定年及其地质意义

朱占平1,刘立1,马瑞1,邱增凯2,马胜晖1   

  1. 1.吉林大学 地球科学学院,长春 130061;2.吉林大学 仪器科学与电气工程学院,长春 130061
  • 收稿日期:2008-08-15 修回日期:1900-01-01 出版日期:2009-03-26 发布日期:2009-03-26
  • 通讯作者: 朱占平

40Ar/39Ar Isotopic Dating and Geological Significance of Mafic Rocks from the Jixi Basin, Heilongjiang Province

ZHU Zhan-ping1, LIU Li1,MA Rui1,QIU Zeng-kai2,MA Sheng-hui1   

  1. 1.College of Earth Sciences, Jilin University, Changchun 130061,China;2.College of Instrumentation & Electrical Engineering, Jilin University, Changchun 130061,China
  • Received:2008-08-15 Revised:1900-01-01 Online:2009-03-26 Published:2009-03-26
  • Contact: ZHU Zhan-ping

摘要: 黑龙江省鸡西盆地张新地区辉绿玢岩呈岩床状侵入晚中生代城子河组地层中;辉绿玢岩较纯净,无捕虏体,呈斑状结构,斑晶由普通辉石、斜长石组成,斑晶体积分数为35%~40%;基质由微晶斜长石、辉石、磁铁矿及玻璃质组成。辉绿玢岩40Ar/39Ar同位素定年结果表明,其等时线年龄与坪年龄在误差范围内较为接近,该辉绿玢岩的形成时代介于96~101 Ma,即形成于早白垩世晚期-晚白垩世早期的Albian-Cenomanian阶。结合区域上该期岩浆事件的特点,暗示早白垩世晚期-晚白垩世时期鸡西盆地处于古太平洋板块(Izanagi-Kula 板块 )向东亚大陆边缘斜向俯冲背景之下的弧后伸展环境。

关键词: 基性岩, 40Ar/39Ar同位素定年, 鸡西盆地

Abstract: The Chengzihe Formation in Zhangxin area of Jixi basin,Heilongjiang Province is intruded by the algorite sill. The mafic rocks are pure, porphyritic and contain no xenolith. The phenocrysts include ordinary augite and plagioclase and make up 35%-40% of the rock. The diabase has same 40Ar/39Ar platform and isochron age of 96-101 Ma within error limit, showing a formation age of the Albian-Cenomanian. Considering the feature of this episode of regional magmatic event, the measured age reveals that the Zhangxin area of the Jixi basin, Heilongjiang Province during the later stage of the Early Cretaceous and Early stage of the Late Cretaceous was under backarc extension within a general tectonic regime of ancient Pacific plate(Izanagi-Kula plate) subduction underneath the East Asia continental plate.

Key words: mafic rock, 40Ar/39Ar isotopic dating, Jixi basin

中图分类号: 

  • P618.13
[1] 蔡益栋, 刘大锰, 姚艳斌, 李俊乾, 郭晓茜, 张百忍. 鸡西盆地煤层气控气地质特征及有利区分布[J]. 吉林大学学报(地球科学版), 2014, 44(6): 1779-1788.
[2] 陈新跃,王岳军,韩会平,张玉芝,温淑女,曹有金. 琼西南三叠纪基性岩脉年代学、地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2014, 44(3): 835-847.
[3] 赵新运,郝立波,陆继龙,赵玉岩,魏俏巧. 红旗岭矿床茶尖矿区铂族元素地球化学特征及其意义[J]. 吉林大学学报(地球科学版), 2013, 43(3): 748-757.
[4] 杨毓红,刘燊,胡瑞忠,冯彩霞,冯光英,杨朝贵,齐有强. 承德三岔口基性岩墙地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1796-1805.
[5] 张永生, 宋天锐, 曹洁, 王俊涛, 苏奎, 樊馥, 龚文强, 刘思宇. 黑龙江东部鸡西盆地首次发现白垩系隐伏含金古砂矿层及其意义[J]. J4, 2010, 40(6): 1278-1286.
[6] 朱占平, 刘立, 马瑞, 邱增凯. 鸡西盆地张新地区浅成侵入体对砂岩储层粘土矿物的影响[J]. J4, 2010, 40(5): 1027-1034.
[7] 任军虎, 柳益群, 周鼎武, 冯乔, 张琨, 董忠良, 秦萍莉. 东昆仑小庙基性岩脉地球化学及LA-ICP-MS锆石U-Pb定年[J]. J4, 2010, 40(4): 859-868.
[8] 高红梅,高福红,樊馥,高玉巧. 鸡西盆地早白垩世烃源岩可溶有机质地球化学特征[J]. J4, 2007, 37(1): 86-0090.
[9] 杨晓平,李仰春,柳 震, 汪 岩,王洪杰. 黑龙江东部鸡西盆地构造层序划分与盆地动力学演化[J]. J4, 2005, 35(05): 616-621.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!