| 注册
首页|期刊导航|地质科学|秦岭商丹带晚中生代同构造花岗岩脉的年代学及其构造意义

秦岭商丹带晚中生代同构造花岗岩脉的年代学及其构造意义

刘园园 李阳 刘钊 陶威 刘富乐 晏山 谭富荣 冉亚洲

地质科学2024,Vol.59Issue(4):889-906,18.
地质科学2024,Vol.59Issue(4):889-906,18.DOI:10.12017/dzkx.2024.064

秦岭商丹带晚中生代同构造花岗岩脉的年代学及其构造意义

Geochronology of Late Mesozoic syn-tectonic granite veins in the Shangdan tectonic belt of the Qinling Orogen and its tectonic implications

刘园园 1李阳 1刘钊 2陶威 3刘富乐 1晏山 1谭富荣 1冉亚洲1

作者信息

  • 1. 西北大学地质学系,大陆动力学国家重点实验室 西安 710069
  • 2. 长庆油田第五采油厂 西安 710200
  • 3. 宿州学院资源与土木工程学院 安徽宿州 234000
  • 折叠

摘要

Abstract

Intense intracontinental orogeny occurred in the Qinling Orogen during Late Mesozoic,and the ages of syn-tectonic granite veins founded in the Shangdan tectonic belt can effectively define the time of intracontinental tectonic deformation.In this paper,zircon U-Pb dating and Hf isotope analysis were conducted on the granite veins.The microstructural observations suggest that the granite veins are characterized by mylonitization,preferred orientation of minerals and medium to high-temperature solid-state deformations,such as the dynamic recrystallization of quartz by grain boundary migration and subgrain rotation,and myrmekite growth textures at the edge of feldspar.CL images reveal that the zircons are marked by spongeous texture with weak cathodoluminescence.Meanwhile,the zircons have lower Th/U ratios in the range of 0.03 to 0.07 and are enriched in heavy rare-elements.According to the discriminant diagrams of(Sm/La)N-La and Ce/Ce*-(Sm/La)N,it can be concluded that the zircons of syn-tectonic granite veins were formed in the transition stage from magmatic to hydrothermal process,belonging to the hydrothermal fluid metasomatic alteration type zircon.Zircon U-Pb dating yields an age of 130~124 Ma for the hydrothermal zircons,representing an important tectonic thermal event.Furthermore,the zircons of granite veins have concentrated negative εHf(t)values of-9.47~-0.99 and Hf two-stage model ages of 1 752~1 218 Ma,probably resulting from the partial melting of the Qinling Group and the Kuanping Group.Combined with previous works,this study reveals that the Yanshanian intracontinental orogeny in Qinling Orogen is characterized by two episodic tectonic deformations,and the age of the syn-tectonic granite veins in Shagoujie ductile shear zone corresponds to the second episode of the intracontinental tectonic deformation.

关键词

同构造花岗岩脉/锆石U-Pb定年/晚中生代/陆内构造变形/秦岭造山带

Key words

Syn-tectonic granite veins/Zircon U-Pb dating/Late Mesozoic/Intracontinental deformation/Qinling Orogen

分类

天文与地球科学

引用本文复制引用

刘园园,李阳,刘钊,陶威,刘富乐,晏山,谭富荣,冉亚洲..秦岭商丹带晚中生代同构造花岗岩脉的年代学及其构造意义[J].地质科学,2024,59(4):889-906,18.

基金项目

国家自然科学基金项目(编号:42172230,41802212)资助 (编号:42172230,41802212)

地质科学

OA北大核心CSTPCD

0563-5020

访问量0
|
下载量0
段落导航相关论文