SEISMOLOGY AND GEOLOGY ›› 1995, Vol. 17 ›› Issue (3): 193-203.

• Brief Report •     Next Articles

THERMAL EVOLUTION HLSTORY AFTER COLLISION OF NORTH CHINA PLATE WITH YANGTZE PLATE

Li Qi1, Chen Wenji1, Ma Balin1, WangQingchen2, Sun Min3   

  1. 1. Institute of Geology, SSB, Beijing 100029;
    2. Institute of Geology, Chinese Academy of Sciences, Beijing 100029;
    3. Department of Earth Sciences, Hong Kong University, Hong Kong
  • Received:1995-05-31 Online:1995-09-06 Published:2009-11-25

华北、扬子板块碰撞后热演化史的初步研究

李齐1, 陈文寄1, 马宝林1, 王清晨2, 孙敏3   

  1. 1. 国家地震局地质研究所, 北京 100029;
    2. 中国科学院地质研究所, 北京 100029;
    3. 香港大学地球科学系, 香港
  • 基金资助:

    国家自然科学基金(49132040)

Abstract:

40Ar-39Ar analyses and MDD(multiple diffusion domain)model treatements were performed for 9 K-feldspar samples.They were collected from gneiss and mylonite of North Jiangsu-Jiaonan-Dabie tectonic melange belt and Tancheng-Lujiang fault zone.The thermal evolution history exhibits five fast ccoling stages found in these samples.In relation with their possible tectonic implications a recovery process after the collision of the North China plate with the Yangtze plate is suggested here.

Key words: Metamorphic belt, Themal history, Geological, Geological age determina-tion, MDD moddel

摘要:

对采自苏北-胶南-大别高压变质构造混杂岩带的片麻岩、糜棱岩和郯庐断裂带上的片麻岩中9个钾长石进行了40Ar-39Ar年龄测定和多重扩散域(MDD)模式处理,9个样品的热演化史表明上述地区存在5个不同的快速冷却时段,并就其可能的构造含义,提出了华北与扬子板块碰撞后的折返历史过程。

关键词: 变质带, 热历史, 地质年代测定, MDD模式