• 全国中文核心期刊
  • 中国科学院引文数据库核心期刊(CSCD)
  • 中国科技核心期刊
  • F5000优秀论文来源期刊
  • 荷兰《文摘与引文数据库》(Scopus)收录期刊
  • 美国《化学文摘》收录期刊
  • 俄罗斯《文摘杂志》收录期刊
高级检索

南天山中段桑树园子韧性剪切带的形成时限及其构造意义

邓松涛, 郭召杰, 张志诚, 廖国辉

邓松涛, 郭召杰, 张志诚, 廖国辉. 南天山中段桑树园子韧性剪切带的形成时限及其构造意义[J]. 中国地质, 2006, 33(3): 641-647.
引用本文: 邓松涛, 郭召杰, 张志诚, 廖国辉. 南天山中段桑树园子韧性剪切带的形成时限及其构造意义[J]. 中国地质, 2006, 33(3): 641-647.
DENG Song-tao, GUO Zhao-jie, ZHANG Zhi-cheng, LIAO Guo-hui. Timing of the formation of the Sangshuyuanzi ductile shear zone in the central segment of the South Tianshan and its tectonic significance[J]. GEOLOGY IN CHINA, 2006, 33(3): 641-647.
Citation: DENG Song-tao, GUO Zhao-jie, ZHANG Zhi-cheng, LIAO Guo-hui. Timing of the formation of the Sangshuyuanzi ductile shear zone in the central segment of the South Tianshan and its tectonic significance[J]. GEOLOGY IN CHINA, 2006, 33(3): 641-647.

南天山中段桑树园子韧性剪切带的形成时限及其构造意义

基金项目: 国家重点基础研究发展规划项目(2001CB40984)资助。

Timing of the formation of the Sangshuyuanzi ductile shear zone in the central segment of the South Tianshan and its tectonic significance

  • 摘要: 提要:南天山中段桑树园子韧性剪切带是一条近东西走向的剪切带,带内面理、线理、不对称构造广泛发育,通过运动学分析判断该剪切带为左旋走滑性质。剪切带内糜棱岩中的白云母40Ar/39Ar测年获得坪年龄(393±6) Ma和等时线年龄(389±3) Ma;带内雁行式裂隙中的黑云母40Ar/39Ar测年获得坪年龄(366.5±2) Ma和等时线年龄(365±3) Ma。结合区域大地构造背景,笔者认为,桑树园子韧性剪切带是由塔里木板块和哈萨克斯坦—伊犁板块斜碰撞产生的同碰撞走滑构造带,在斜碰撞过程中起到平行板块边界方向的应变分解作用。
    Abstract: Abstract:The Sangshuyuanzi ductile shear zone in the central segment of the South Tianshan is an east-west-trending shear zone, in which foliations, lineations and asymmetric structures are well developed. Based on a kinematic analysis,the authors think that the Sangshuyuanzi ductile shear zone is of sinistral strike-slip nature. 40Ar/39Ar dating of muscovites from mylonite in the shear zone yields a plateau age of 393±6 Ma and an isochron age at 389±3 Ma. 40Ar/39Ar dating of biotites from en-echelon fractures in the zone gives a plateau age of 366.5±2 Ma and an isochron age of 365.0±3 Ma. According to the above-mentioned study, combined with the regional tectonic background, this paper suggests that the Sangshuyuanzi ductile shear zone is a syncollisional strike-slip tectonic zone formed by oblique collision between the Tarim plate and the Kazakhstan-Ili plate, which resulted in strain partitioning parallelly to the boundary of the two plates.
计量
  • 文章访问数:  2862
  • HTML全文浏览量:  53
  • PDF下载量:  2723
  • 被引次数: 0
出版历程
  • 刊出日期:  2006-06-24

目录

    /

    返回文章
    返回
    x 关闭 永久关闭