青藏高原东南部及三江地区新生代构造隆升 ——来自裂变径迹热史反演分析

金维浚, 何登发, 雷振宇, 孔祥儒. 青藏高原东南部及三江地区新生代构造隆升 ——来自裂变径迹热史反演分析[J]. 地质科学, 2012, 47(3): 714-729.
引用本文: 金维浚, 何登发, 雷振宇, 孔祥儒. 青藏高原东南部及三江地区新生代构造隆升 ——来自裂变径迹热史反演分析[J]. 地质科学, 2012, 47(3): 714-729.
Jin Weijun, He Dengfa, Lei Zhenyu, Kong Xiangru. Uplift of southeastern Tibet and Sanjiang area during Cenozoic era ——Thermal inversion analysis from fission track data[J]. Chinese Journal of Geology, 2012, 47(3): 714-729.
Citation: Jin Weijun, He Dengfa, Lei Zhenyu, Kong Xiangru. Uplift of southeastern Tibet and Sanjiang area during Cenozoic era ——Thermal inversion analysis from fission track data[J]. Chinese Journal of Geology, 2012, 47(3): 714-729.

青藏高原东南部及三江地区新生代构造隆升 ——来自裂变径迹热史反演分析

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    作者简介:

    金维浚, 男, 1963年1月生, 博士, 副研究员, 构造地质学和勘探地球物理学专业。E-mail: wjjin@mail.iggcas.ac.cn

  • 中图分类号: P542

Uplift of southeastern Tibet and Sanjiang area during Cenozoic era ——Thermal inversion analysis from fission track data

  • 通过对青藏高原东南部及三江地区8个样品磷灰石和锆石裂变径迹分析、热史反演,对这一地区构造运动及隆升作用进行定量分析。表明青藏高原东南部新生代以来经历两次构造抬升期,在50 Ma和6~5 Ma,其特点是早期为缓慢隆升; 晚期为快速抬升期,抬升速率为0.5 mm/a。位于三江地区扬子地块的楚雄盆地构造隆升受青藏高原隆升的影响,受盆地中部构造和古隆起影响,盆地东西部次级坳陷在120~60 Ma 表现为相反垂向运动趋势,盆地表现为50 Ma左右有一次相一致抬升运动趋势。总结本区裂变径迹年龄及长度分布规律,表明北东向构造分界明显,可能是印度地块与冈底斯地块碰撞后在东南无约束边界条件下侧向扩展形成。
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出版历程
收稿日期:  2012-04-10
修回日期:  2012-05-24
刊出日期:  2012-07-25

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