新疆叶尔羌河上游全新世阶地的释光年代与河流下切速率

doi:10.3969/j.issn.0253-4967.2011.02.015

地震地质 ›› 2011, Vol. 33 ›› Issue (2): 421-429.DOI: 10.3969/j.issn.0253-4967.2011.02.015

新疆叶尔羌河上游全新世阶地的释光年代与河流下切速率

刘进峰, 陈杰, 王昌盛

中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029

收稿日期:2011-04-26 修回日期:2011-05-31 出版日期:2011-06-29 发布日期:2011-12-17
作者简介:刘进峰,男,1977年生,2005年在中国科学院地质与地球物理研究所获博士学位,副研究员,主要研究方向为新构造与释光年代学,电话: 010-62009038,E-mail: liujf81@ies.ac.cn。
基金资助:
地震动力学国家重点实验室自主研究课题(LED2010A04)、科技部国际科技合作计划项目(2008DFA20860)和地震行业科研专项(200808015)共同资助

OPTICAL DATING OF THE HOLOCENE TERRACE SEDIMENTS AND THE INCISION RATE IN THE UPPER REACH OF THE YARKANT RIVER IN XINJIANG

LIU Jin-feng, CHEN Jie, WANG Chang-sheng

State Key Laboratory of Earthquake Dynamics,Institute of Geology, China Earthquake Administration,Beijing 100029,China

Received:2011-04-26 Revised:2011-05-31 Online:2011-06-29 Published:2011-12-17

摘要/Abstract

摘要：

采用细颗粒石英简单多片再生法对新疆叶尔羌河上游阶地进行了光释光测年,并在不同实验室进行了等效剂量对比测试,结果基本一致。测年结果显示,该阶地沉积形成于距今4.3～7.3ka,自阶地形成以来,河流下切(27±5)m,下切速率(6.3±1.2)mm/a。塔什库尔干河中上游河流的快速下切可能与慕士塔格山穹窿的快速隆升或第四纪冰川作用有关。

关键词: 河流阶地, 光释光测年, 叶尔羌河, 下切速率

Abstract:

The Tashkurgan-Yarkant River,which is the upper reach of the Tarim River,originates from the Karakoram Mountains in the west syntaxis of the Tibetan Plateau.Thick terrace sediments are widespread along the Tashkurgan-Yarkant River.These deposits contain geologic fingerprints that allow identification of the environmental changes and geologic hazards.However,few geochronological data was available on these sedimentations to allow us to build an irreproachable age model.4 samples of fine grains from one terrace profile were dated by optically stimulated luminescence(OSL)dating method.In darkroom,fractions of fine grains(4～11μm)were extracted from the bulk samples.OSL signal measurements were performed on an automated Daybreak system.Identical D_e plateau in the thermal treat was observed in preheat plateau test.Tests of luminescence characteristics confirm the suitability of the material for OSL dating.Our results indicate the deposition age for these sediments is between 4.3～7.3ka.After the river terrace deposited,the river has deeply incised for 27±5m,with the incision rate 6.3±1.2mm/a.The thermochronologic data show that the magnitude of exhumation decreases from upstream(west)to downstream(east)along the Tashkurgan-Yarkand River.These data may reflect the the active uplift process of Mustagh Ata antiform.

Key words: River terrace, OSL dating, Tashkurgan-Yarkant River, River incision rate

中图分类号:

P315.2

刘进峰, 陈杰, 王昌盛. 新疆叶尔羌河上游全新世阶地的释光年代与河流下切速率[J]. 地震地质, 2011, 33(2): 421-429.

LIU Jin-feng, CHEN Jie, WANG Chang-sheng. OPTICAL DATING OF THE HOLOCENE TERRACE SEDIMENTS AND THE INCISION RATE IN THE UPPER REACH OF THE YARKANT RIVER IN XINJIANG[J]. SEISMOLOGY AND GEOLOGY, 2011, 33(2): 421-429.

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新疆叶尔羌河上游全新世阶地的释光年代与河流下切速率

OPTICAL DATING OF THE HOLOCENE TERRACE SEDIMENTS AND THE INCISION RATE IN THE UPPER REACH OF THE YARKANT RIVER IN XINJIANG

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