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内蒙古东部索伦二叠纪哲斯组碎屑锆石U-Pb年龄及其大地构造意义
  • ISSN号:1671-1815
  • 期刊名称:《科学技术与工程》
  • 时间:0
  • 分类:P595.26[天文地球—地球化学;天文地球—地质学]
  • 作者机构:[1]吉林大学地球科学学院,长春130061
  • 相关基金:国家自然科学基金项目(40872121)、国家发改委油气专项(14809XQl021)资助
作者: 李雨柯[1]
中文摘要:

内蒙古索伦地区位于贺根山-黑河断裂和西拉木伦河一长春一延吉断裂之间,该区发育巨厚的二叠系哲斯组地层。研究其年代学特征对确定该区大地构造背景具有重要的指示意义。哲斯组50颗碎屑锆石镜下具有典型岩浆锆石特征,年代学记录表现为4个峰值:(1)[(2704-2)一(335±4)]Ma,峰期年龄为(2724-2)Ma,与该区晚古生代岩浆活动一致;(2)[(363±3)-(429±3)]Ma,峰期年龄为(382±4)Ma,暗示其物源来自于松辽地块及其周边地区的加里东期岩浆事件;(3)[(507±5)~(555±6)]Ma,峰期年龄为(515±3)Ma,与东北地区各地块的泛非期变质基底年龄一致;(4)少量前寒武纪年龄分别为(847±7)Ma、(923±7)Ma、(1342±14)Ma、(2040±13)Ma,表明东北地区存在元古宙的结晶基底。上述碎屑锆石的年代学研究表明,以泛非期和新元古事件年龄为代表,说明研究区哲斯组的物源应来源于东北地区的变质基底,其中年轻一组谐和年龄(270±2)Ma限定了哲斯组的沉积下限为晚二叠世。由于哲斯组的物源均来自于东北地区的变质基底,推测华北和西伯利亚板块的缝合位置在西拉木伦河一长春一延吉一线。

英文摘要:

Located in the between of Hegenshan-Heihe fault and Xar Moron River-Changchun-Yanji fault in In- ner Mongolia, Suolun exist thick Permian Zhesi Formation , and there is an important significance with instructions to determine the tectonic setting for the Chronological characteristics of Zhesi Formation. 50 detrital zircon geochro- nology study of Zhesi Formation displays four peaks with typical features of magmatic zircons : ( 1 ) [ (270 ± 2 ) ± (335 ± 4) ] Ma with the peak age at (272 ± 2) Ma being identical with Late Paleozoic magmatism; (2) [ (363 ± 3 ) (429 ±3) ] Ma with the peak age at (382 ±4) Ma showing that the provenance comes from Caledonian magmatic events of Songliao Block and its surrounding areas; (3) [ (507 ±5) ± (555 ±6) ] Ma with the peak age at (515 ± 3 ) Ma corresponding to Pan-African age of the metamorphic basement in the Northeast China Block ; (4) ( 847 ± 7 ) Ma, (923 ±7) Ma, ( 1 342 ± 14) Ma, (2 040 ± 13) Ma in Precambrian showing that there is Proterozoic crystalline basement in the Northeast China Block. On behalf of the age of Pan-African event, above-mentioned detrital zircon geochronology study shows that the provenance of Zhesi Formation should come from metamorphic basement of the the Northeast China Block in the study area, and the young concordia age is (270 ± 2) Ma which shows that the deposition of lower age should be Late Permian. Because the provenance of Zhesi Formation comes from metamor- phic basement of the Northeast China Block, so the suture zone between the Siberia Plate and North China Plate may be the Xar Moron River-Changchun-Yanji fault.

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期刊信息
  • 《科学技术与工程》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学技术协会
  • 主办单位:中国技术经济学会
  • 主编:明廷华
  • 地址:北京市学院南路86号
  • 邮编:100081
  • 邮箱:ste@periodicals.net.cn
  • 电话:010-62118920
  • 国际标准刊号:ISSN:1671-1815
  • 国内统一刊号:ISSN:11-4688/T
  • 邮发代号:2-734
  • 获奖情况:
  • 国内外数据库收录:
  • 中国中国科技核心期刊,中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:29478