北京延庆盆地50万年以来的主要构造事件及年代学的初步研究

尹功明; 卢演俦

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北京延庆盆地50万年以来的主要构造事件及年代学的初步研究

尹功明, 卢演俦

文章导航 > 华北地震科学 > 1996 > 14(4): 19-30

尹功明, 卢演俦. 北京延庆盆地50万年以来的主要构造事件及年代学的初步研究[J]. 华北地震科学, 1996, 14(4): 19-30.

引用本文:

尹功明, 卢演俦. 北京延庆盆地50万年以来的主要构造事件及年代学的初步研究[J]. 华北地震科学, 1996, 14(4): 19-30.

Yin Gongming, Lu Yanchou. THE QUATERNARY TECTONIC EVENTS IN THE YANQING FAULTING-DOWN BASIN, BEIJING[J]. North China Earthquake Sciences, 1996, 14(4): 19-30.

Citation:

Yin Gongming, Lu Yanchou. THE QUATERNARY TECTONIC EVENTS IN THE YANQING FAULTING-DOWN BASIN, BEIJING[J]. North China Earthquake Sciences, 1996, 14(4): 19-30.

北京延庆盆地50万年以来的主要构造事件及年代学的初步研究

国家地震局地质研究所, 北京 100029

基金项目: 地震科学联合基金85080701课题资助;国家地震局地质研究所论著96C0010

详细信息

中图分类号: P542

THE QUATERNARY TECTONIC EVENTS IN THE YANQING FAULTING-DOWN BASIN, BEIJING

Institute of Geology, State Seismological Bureau, Beijing 100029

摘要: 延庆盆地是一个位于燕山山脉南部的晚新生代形成的小型断陷盆地,通过对延庆盆地系统的野外调查,根据延庆盆地的地貌、沉积物、断裂活动等特征,初步认为延庆盆地在过去约50万年曾发生过三次对盆地地貌和沉积环境演化发生过重要影响或改变盆地演化过程的重大构造事件。针对上述三次构造事件,采集了适当的测年样品,经电子自旋共振(ESR)、红外释光(OSL)测年技术等测定,得出了延庆盆地三次主要构造事件发生的可能年代,分别发生在距今40万年-35万年、距今15万年-10万年和距今1.8万年-1.2万年。
- 延庆-怀来盆地 /
- 构造分析 /
- 第四纪
Abstract: The Yanqing faulting-down basin, with NEE extension, is located at the southern margin of Yan-shan Mountain. The basin has developed since the late Cenozoic, and can be regarded as one of the tension basins in the northeastern tip of Shanxi shear faulting zone. According to detailed investigation of landform evolution and sedimentation variation, a compendium outline of neotectonic deformation of the basin has been suggested as fellows. There were three major tectonic events which controlled the evolution of the basin in 500ka B. P.. It is confirmed that the oldest one of lake sediments which were exposed on the surface in the basin was accumulated in the middle Pleistocene. The first event occurred in the middle period of Middle Pleistoncence and its distinguishing feature is the slipping down of the northern margin fault and the uplifting of the entire basin again. The second event took place between Middle and Late Pleistocene, representing uplifting of the basin and the around mountains, and re-action of normal faulting along the northern margin. The third event occurred in the late period of Late Pleistocene and has the similar features to the second one. Many proper samples for dating of the three events mentioned above were collected. Based on ESR dating, TL dating, IRSL dating and ¹⁴C dating of the samples, age estimates of the three events have been obtained as fellows: the first event in 0.40-0.35 ma BP., the second event in 0.15-0.10 ma BP. and the third event in 18-12 ka BP. respectively.
- Yanqing Baisn /
- Tectonic event /
- Quaternary

[1]

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北京延庆盆地50万年以来的主要构造事件及年代学的初步研究

国家地震局地质研究所, 北京 100029

基金项目: 地震科学联合基金85080701课题资助;国家地震局地质研究所论著96C0010

收稿日期: 1996-03-10
刊出日期: 1996-12-15

中图分类号: P542

关键词:

延庆-怀来盆地 /

构造分析 /

第四纪

摘要: 延庆盆地是一个位于燕山山脉南部的晚新生代形成的小型断陷盆地,通过对延庆盆地系统的野外调查,根据延庆盆地的地貌、沉积物、断裂活动等特征,初步认为延庆盆地在过去约50万年曾发生过三次对盆地地貌和沉积环境演化发生过重要影响或改变盆地演化过程的重大构造事件。针对上述三次构造事件,采集了适当的测年样品,经电子自旋共振(ESR)、红外释光(OSL)测年技术等测定,得出了延庆盆地三次主要构造事件发生的可能年代,分别发生在距今40万年-35万年、距今15万年-10万年和距今1.8万年-1.2万年。

English Abstract

THE QUATERNARY TECTONIC EVENTS IN THE YANQING FAULTING-DOWN BASIN, BEIJING

Institute of Geology, State Seismological Bureau, Beijing 100029

Received Date: 1996-03-10
Publish Date: 1996-12-15

Keywords:

Abstract: The Yanqing faulting-down basin, with NEE extension, is located at the southern margin of Yan-shan Mountain. The basin has developed since the late Cenozoic, and can be regarded as one of the tension basins in the northeastern tip of Shanxi shear faulting zone. According to detailed investigation of landform evolution and sedimentation variation, a compendium outline of neotectonic deformation of the basin has been suggested as fellows. There were three major tectonic events which controlled the evolution of the basin in 500ka B. P.. It is confirmed that the oldest one of lake sediments which were exposed on the surface in the basin was accumulated in the middle Pleistocene. The first event occurred in the middle period of Middle Pleistoncence and its distinguishing feature is the slipping down of the northern margin fault and the uplifting of the entire basin again. The second event took place between Middle and Late Pleistocene, representing uplifting of the basin and the around mountains, and re-action of normal faulting along the northern margin. The third event occurred in the late period of Late Pleistocene and has the similar features to the second one. Many proper samples for dating of the three events mentioned above were collected. Based on ESR dating, TL dating, IRSL dating and ¹⁴C dating of the samples, age estimates of the three events have been obtained as fellows: the first event in 0.40-0.35 ma BP., the second event in 0.15-0.10 ma BP. and the third event in 18-12 ka BP. respectively.

尹功明, 卢演俦. 北京延庆盆地50万年以来的主要构造事件及年代学的初步研究[J]. 华北地震科学, 1996, 14(4): 19-30.

引用本文:

尹功明, 卢演俦. 北京延庆盆地50万年以来的主要构造事件及年代学的初步研究[J]. 华北地震科学, 1996, 14(4): 19-30.

Yin Gongming, Lu Yanchou. THE QUATERNARY TECTONIC EVENTS IN THE YANQING FAULTING-DOWN BASIN, BEIJING[J]. North China Earthquake Sciences, 1996, 14(4): 19-30.

Citation:

Yin Gongming, Lu Yanchou. THE QUATERNARY TECTONIC EVENTS IN THE YANQING FAULTING-DOWN BASIN, BEIJING[J]. North China Earthquake Sciences, 1996, 14(4): 19-30.