断层物质测年的热释光研究

地震地质 ›› 1994, Vol. 16 ›› Issue (2): 167-175.

断层物质测年的热释光研究

计凤桔¹, 马胜利¹, 刘明达²

1. 国家地震局地质研究所, 北京 100029;
2. 国家地震局地壳应力研究所, 北京 100085

收稿日期:1991-11-01 修回日期:1992-09-01 出版日期:1994-06-08 发布日期:2009-11-25

STUDY OF FAULT GOUGE DATING USING TL TECHNIQUE

Ji Fengju¹, Ma Shengli¹

1. Institute of Geology, SSB, Beijing 100029;
2. Institute of Crustal Dynamics, SSB, Beijing 100085

Received:1991-11-01 Revised:1992-09-01 Online:1994-06-08 Published:2009-11-25

摘要/Abstract

摘要：

断层物质TL测年的关键,是断裂运动产生的温压效应能否使断裂带内某些矿物原贮存的TL能量完全释放而“归零”。为此,进行了不同条件的高温、高压和位移速率变化等的模拟断裂运动的实验。结果表明,断裂运动产生的摩擦增温是使断层面上矿物TL强度减弱的主要因素。讨论了摩擦增温值与断裂运动时剪应力大小、断层泥厚度和断层位移间的关系,并得到了野外断层面上实际测试的证实。据此研究成果,还对小湾坝区F₇断裂的活动时代进行了测定。

关键词: TL退火, 摩擦增温, 断层泥厚度, 位移距离, 剪应力

Abstract:

The key to the question about fault gouge dating by TL technique is whether the temperature and pressure effect caused by faulting can lead the origional TL to“zoro”for some minerals.For this purpose,we have made the simulated experiments under different temperature,pressureand strain rate which can lead TL intensity of quartz in fault zone to decrease.The results showthat the frictional heating by dislocation of fault walls during faulting is a main factor leading thequartz TL to decrease on the fault plane and that increment of temperature is closely related withthe value of shear stress,gouge thickness and displacements,and it is confirmed by the measurements of fault gouge on the plane.According to above reseach,the time of activity has been dated along F₇ fault at Xiaowan,Yunnan province.

Key words: TL annealing, Frctional heating, Thickness of fault gouge, Displacement, Shear stress

计凤桔, 马胜利, 刘明达. 断层物质测年的热释光研究[J]. 地震地质, 1994, 16(2): 167-175.

Ji Fengju, Ma Shengli. STUDY OF FAULT GOUGE DATING USING TL TECHNIQUE[J]. SEISMOLOGY AND GEOLOGY, 1994, 16(2): 167-175.

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