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高校地质学报 ›› 2023, Vol. 29 ›› Issue (6): 872-885.DOI: 10.16108/j.issn1006-7493.2022057

• 构造地质学 • 上一篇    下一篇

青藏高原东缘中新生代隆升及构造扩展方式转换

金文正1, 2,白万奎3,叶治续4   

  1. 1. 中国地质大学(北京)能源学院,北京 100083;
    2. 油气资源与探测国家重点实验室,北京 102249;
    3. 中国石化胜利油田分公司物探研究院,东营 257000;
    4. 中国石油天然气股份有限公司冀东油田分公司,唐山 063200
  • 出版日期:2023-12-20 发布日期:2023-12-18

Meso-Cenozoic Uplift and Transformation of Tectonic Extension Mode in the Eastern Margin of Qinghai-Tibet Plateau

JIN Wenzheng1,2,BAI Wankui3,YE Zhixu4   

  1. 1. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
    2. State Key Laboratory for Petroleum Resource and Prospecting, Beijing 102249, China;
    3. Geophysical Research Institute of Sinopec Shengli Oilfield Branch, Dongying 257000, China;
    4. Jidong Oilfield Branch Company, PetroChina, Tangshan 063200, China
  • Online:2023-12-20 Published:2023-12-18

摘要: 为研究青藏高原向东构造挤压过程中,构造变形扩展方式的变化,文章选取青藏高原东缘为研究对象,开展了磷灰石和锆石裂变径迹测定及分析工作。结果表明,若尔盖盆地和龙门山块体具有诸多低温热年代学及构造隆升差异:若尔盖盆地样品冷却速率较为集中,介于1.257~1.285 ℃/Myr,而龙门山块体样品冷却速率变化较大,介于1.243~2.875 ℃/Myr;若尔盖盆地在100 Ma以来共经历了2次明显的构造热事件,第一次为100~80 Ma(冷却速率为4.40±0.395 ℃/Myr),第二次为21~12 Ma(冷却速率为2.89±0.597 ℃/Myr),龙门山块体东缘地区在70 Ma以来,总体上表现为构造隆升程度的逐渐增强,且在8 Ma以来构造隆升持续增强,冷却速率达到了5.75±0.238 ℃/Myr;若尔盖盆地的构造变形属于前展式构造扩展,而龙门山块体则为后展式(自8 Ma以来),文章将该过程总结为“构造变形扩展的反射和折射”现象,“反射部分”在第四纪(4.48 Ma)达到龙日坝断裂附近,形成兼具逆冲与右旋走滑的龙日坝断裂带。

关键词: 裂变径迹, 前展式, 后展式, 构造隆升, 青藏高原

Abstract: In order to analyze changes in of tectonic deformation and extension mode during the process of eastward compression of Qinghai-Tibet Plateau, the eastern edge of Qinghai-Tibet Plateau is selected as the study area, and apatite/zircon fission track studies were carried out. The results show that many differences between the Zoige Basin and the Longmenshan Block in the aspect of low-temperature geochronology and tectonic uplift: the cooling rates of several samples in the Zoige basin are relatively stable, ranging from 1.257 ℃ to 1.285 ℃ /Myr, while the cooling rates of several samples in the Longmenshan Block changes greatly, ranging from 1.243 ℃ to 2.875 ℃ /Myr; Zoige Basin has experienced two obvious tectonic thermal events since 100 Ma with the first in 100-80 Ma (cooling rate is 4.40±0.395 ℃ /Myr) and the second in 21-12 Ma (cooling rate is 2.89±0.597 ℃ /Myr). The eastern edge of Longmenshan Block has generally shown a gradual increase in the degree of tectonic uplift since 70 Ma, and the uplift has continued to increase since 8 Ma with the cooling rate of 5.75±0.238 ℃ /Myr; The tectonic deformation of Zoige Basin can be classified as forward expansion, while the Longmenshan Block has backward expansion (especially since 8 Ma). The process mentioned above is summarized a“s reflection and refraction of tectonic expansion”, the“ reflection tectonic stress”reached current location of Longriba fault in Pliocene (about 4.48 Ma), with the result of the Longriba fault zone with the features of both thrust and dextral strike slip.

Key words: fission track, piggyback propagation, overstep propagation, tec tonic uplift, Qinghai-Tibet Plateau

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