安丘-莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究

范军; 翟正宏; 管延新; 刘世友; 李栋梁; 熊玮

doi:10.3969/j.issn.1003-1375.2015.01.008

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安丘-莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究

范军, 翟正宏, 管延新, 刘世友, 李栋梁, 熊玮

文章导航 > 华北地震科学 > 2015 > 33(1): 39-45

范军, 翟正宏, 管延新, 刘世友, 李栋梁, 熊玮. 安丘-莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究[J]. 华北地震科学, 2015, 33(1): 39-45. doi: 10.3969/j.issn.1003-1375.2015.01.008

引用本文:

FAN Jun, ZHAI Zheng-hong, GUAN Yan-xin, LIU Shi-you, LI Dong-liang, XIONG Wei. Spatial Location and Activity Research on the North Section of Anqiu-Juxian Fault and Changyi-Dadian Fault From Zhuli[J]. North China Earthquake Sciences, 2015, 33(1): 39-45. doi: 10.3969/j.issn.1003-1375.2015.01.008

Citation:

FAN Jun, ZHAI Zheng-hong, GUAN Yan-xin, LIU Shi-you, LI Dong-liang, XIONG Wei. Spatial Location and Activity Research on the North Section of Anqiu-Juxian Fault and Changyi-Dadian Fault From Zhuli[J]. North China Earthquake Sciences, 2015, 33(1): 39-45. doi: 10.3969/j.issn.1003-1375.2015.01.008

安丘-莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究

doi: 10.3969/j.issn.1003-1375.2015.01.008

1.
潍坊市地震局, 山东潍坊 261061;
2.
安丘地震台, 山东潍坊 262100

基金项目: 山东省地震局合同制科研项目(13Y19)

详细信息

作者简介:
范军(1981—),男(汉族),山东潍坊人,助理工程师,主要从事地震监测预报和地震信息网络管理.E-mail:fj900@163.com

中图分类号: P135.242

Spatial Location and Activity Research on the North Section of Anqiu-Juxian Fault and Changyi-Dadian Fault From Zhuli

1.
Earthquake Administration of Weifang, Shandong Weifang 261061, China;
2.
Anqiu Seismic station, Shandong Weifang 262100, China

摘要: 安丘-莒县断裂与昌邑-大店断裂朱里以北段,主要隐伏于第四系之下,少见断裂出露。本项研究根据近年来开展的大量地球物理探测成果,结合野外地质考察、钻探验证以及断层活动资料等的分析对比,阐述了安丘-莒县断裂与昌邑-大店断裂的空间位置和构造特征,并应用区域地震地质、第四纪地质方法和断裂活动的绝对年龄资料对断裂现代活动性进行研究,认为安丘-莒县断裂主要经方家屯村东、文山东坡、石湾店南村西、东冢镇后柳村东、下营等地,属晚更新世活动断裂;昌邑-大店断裂作为郯庐断裂带东地堑的东侧边界断裂,控制潍河东侧的青山、青龙山花岗岩体的西边界,经董家隅村东、下营东,向北大致与安丘莒县断裂平行延伸至莱州湾,属于早中更新世断裂。
- 空间位置 /
- 断裂活动性 /
- 安丘-莒县断裂 /
- 昌邑-大店断裂 /
- 昌邑
Abstract: The north section of Anqiu-Juxian fault and Changyi-Dadian fault from Zhuli is mostly concealed under the Quaternary system and has little outcrops. On the basis of a large number of geophysical detection results in recent years, combining with the field geological investigation, drilling verification and comparison analysis of fault activity information, this study expounds the location and structure characteristic of the Anqiu-Juxian fault and the Changyi-Dadian fault, studies the modern fracture activity using the method of seismic geology and quaternary geology based on absolute age data. The results show that the Anqiu-Juxian fault mainly cuts across the northern Fangjatun village, eastern slope of Wenshan, western Shiwandian-south viilage, eastern Houliu village of Dongzhong town and Xiaying village, etc. and is a late Pleistocene active fault. As the eastern boundary faults of the east-graben on the east of the Tanlu fault zone, the Changyi-Dadian fault controls the west boundry of granite rock mass of Qingshan and Qinglongshan in the east side of the Weihe. The Changyi-Dadian fault goes across the east side of Dongjia village, eastern Xiaying and extends to the Laizhou Bay; it is nearly parallel to the Anqiu-Juian fault to northward and is an early Pleistocene fault.
- spatial location /
- fault activity /
- Anqiu-Juxian fault /
- Changyi-Dadian fault /
- Changyi

[1]	国家地震局地质研究所.郯庐断裂[M].北京: 地震出版社,1987.
[2]	李家灵,晁洪太,崔昭文,等.郯城活断层的分段及其大震危险性分析[J].地震地质,1994,16(2):45-50.
[3]	魏光兴.郯庐带地震活动性研究[M].北京: 地震出版社,1993.
[4]	中国地震局.中国地震活动断层探测技术系统技术规程[S].北京:地震出版社,2005:3-42.
[5]	高维明,李家灵,孙竹友.沂沭大陆裂谷的生成与演化[J].地震地质,1980,2(3):11-18.
[6]	晁洪太,李家灵,崔昭文,等.郯庐断裂带中段全新世活断层的几何结构与分段[M].国家地震局地质研究所.活动断裂研究(3).北京:地震出版社,1994,180-190.
[7]	晁洪太,李家灵,崔昭文,等.郯庐断裂带中段全新世活断层的特征滑动行为与特征地震[J].内陆地震, 1994b,8(4):297-304.
[8]	高维明,郑郞荪,李家灵,等.1668年山东郯城8.5级地震的发震构造[J].中国地震,1988,4(3):9-15.
[9]	王华林.公元前70年诸城-昌乐地震发震构造的初步研究.地震学刊, 1990,(3): 100-130.
[10]	夏东兴,刘振夏,吴桑云,等.末次冰期黄河解体事件初探[J].海洋与湖沼, 1996,27(5):511-517.
[11]	杨一冲,高维明.沂沭活断层北段F1断层滑动方式的讨论[J].地震地质,1994,16(1):12-20.
[12]	管延新,翟正宏,李宗贤,等.沂沭断裂带安丘-莒县断裂昌邑段空间分布特征和活动性分析[J].海洋地质动态,2007,23(2):17-19.

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[5]	周海涛, 郭良迁, 张立成. 唐山断裂现代活动性研究 . 华北地震科学, 2009, 27(3): 17-22.
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[7]	李愿军, 丁美英. 关于高桥断裂及其活动性的讨论 . 华北地震科学, 1995, 13(1): 1-8.
[8]	方仲景, 段瑞涛, 郑炳华, 杨主恩. 河北省怀安盆地北缘断裂活动性研究 . 华北地震科学, 1994, 12(4): 25-33.
[9]	杜广仁. 从鹤壁地区岩浆活动与断裂的关系探讨地震活动性 . 华北地震科学, 1993, 11(3): 62-69.
[10]	李文浩, 向宏发, 方仲景, 李如成, 张晚霞. 密云-前门隐伏断裂活动性的初步研究 . 华北地震科学, 1992, 10(2): 43-49.

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安丘-莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究

doi: 10.3969/j.issn.1003-1375.2015.01.008

1. 潍坊市地震局, 山东潍坊 261061;

2. 安丘地震台, 山东潍坊 262100

基金项目: 山东省地震局合同制科研项目(13Y19)

作者简介:
范军(1981—),男(汉族),山东潍坊人,助理工程师,主要从事地震监测预报和地震信息网络管理.E-mail:fj900@163.com

收稿日期: 2014-11-03
刊出日期: 2015-03-15

中图分类号: P135.242

关键词:

摘要: 安丘-莒县断裂与昌邑-大店断裂朱里以北段,主要隐伏于第四系之下,少见断裂出露。本项研究根据近年来开展的大量地球物理探测成果,结合野外地质考察、钻探验证以及断层活动资料等的分析对比,阐述了安丘-莒县断裂与昌邑-大店断裂的空间位置和构造特征,并应用区域地震地质、第四纪地质方法和断裂活动的绝对年龄资料对断裂现代活动性进行研究,认为安丘-莒县断裂主要经方家屯村东、文山东坡、石湾店南村西、东冢镇后柳村东、下营等地,属晚更新世活动断裂;昌邑-大店断裂作为郯庐断裂带东地堑的东侧边界断裂,控制潍河东侧的青山、青龙山花岗岩体的西边界,经董家隅村东、下营东,向北大致与安丘莒县断裂平行延伸至莱州湾,属于早中更新世断裂。

English Abstract

Spatial Location and Activity Research on the North Section of Anqiu-Juxian Fault and Changyi-Dadian Fault From Zhuli

1. Earthquake Administration of Weifang, Shandong Weifang 261061, China;

2. Anqiu Seismic station, Shandong Weifang 262100, China

Received Date: 2014-11-03
Publish Date: 2015-03-15

Keywords:

Abstract: The north section of Anqiu-Juxian fault and Changyi-Dadian fault from Zhuli is mostly concealed under the Quaternary system and has little outcrops. On the basis of a large number of geophysical detection results in recent years, combining with the field geological investigation, drilling verification and comparison analysis of fault activity information, this study expounds the location and structure characteristic of the Anqiu-Juxian fault and the Changyi-Dadian fault, studies the modern fracture activity using the method of seismic geology and quaternary geology based on absolute age data. The results show that the Anqiu-Juxian fault mainly cuts across the northern Fangjatun village, eastern slope of Wenshan, western Shiwandian-south viilage, eastern Houliu village of Dongzhong town and Xiaying village, etc. and is a late Pleistocene active fault. As the eastern boundary faults of the east-graben on the east of the Tanlu fault zone, the Changyi-Dadian fault controls the west boundry of granite rock mass of Qingshan and Qinglongshan in the east side of the Weihe. The Changyi-Dadian fault goes across the east side of Dongjia village, eastern Xiaying and extends to the Laizhou Bay; it is nearly parallel to the Anqiu-Juian fault to northward and is an early Pleistocene fault.

引用本文:

Citation:

FAN Jun, ZHAI Zheng-hong, GUAN Yan-xin, LIU Shi-you, LI Dong-liang, XIONG Wei. Spatial Location and Activity Research on the North Section of Anqiu-Juxian Fault and Changyi-Dadian Fault From Zhuli[J]. North China Earthquake Sciences, 2015, 33(1): 39-45. doi: 10.3969/j.issn.1003-1375.2015.01.008