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[1]刘 洁,李 营,陈 志,等.陇县—宝鸡断裂带CO2气体地球化学特征及成因[J].地震研究,2022,45(02):217-228.[doi:10.20015/j.cnki.ISSN1000-0666.2022.0020 ]
 LIU Jie,LI Ying,CHEN Zhi,et al.Geochemical Characteristics and Genesis of Soil Gas CO2 in the Longxian-Baoji Fault Zone[J].Journal of Seismological Research,2022,45(02):217-228.[doi:10.20015/j.cnki.ISSN1000-0666.2022.0020 ]
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陇县—宝鸡断裂带CO2气体地球化学特征及成因(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
45
期数:
2022年02期
页码:
217-228
栏目:
出版日期:
2022-05-20

文章信息/Info

Title:
Geochemical Characteristics and Genesis of Soil Gas CO2 in the Longxian-Baoji Fault Zone
作者:
刘 洁1李 营2陈 志2王 新1赵小茂1冯希杰1王景丽1
(1.陕西省地震局,陕西 西安 710068; 2.中国地震局地震预测研究所 中国地震局地震预测重点实验室,北京 100036)
Author(s):
LIU Jie1LI Ying2CHEN Zhi2WANG Xin1ZHAO Xiaomao1FENG Xijie1WANG Jingli1
(1.Shaanxi Earthquake Agency,Xi'an 710068,Shaanxi,China)(2.Institute of Earthquake Forecasting and Key Laboratory of Earthquake Prediction,China Earthquake Administration,Beijing 100036,China)
关键词:
土壤气CO2 气体活动强度 碳稳定同位素 断层活动性
Keywords:
soil gas CO2 intensity of gas activity stable carbon isotope fault activity
分类号:
P315.724
DOI:
10.20015/j.cnki.ISSN1000-0666.2022.0020
摘要:
陇县—宝鸡断裂带位于青藏块体东北缘,属于鄂尔多斯块体西南缘弧形断裂束的最南段。为对比分析该断裂带的分段活动性强弱特征,利用断裂带逸出气CO2的地球化学特征进行反演。布设6条跨断层土壤气CO2测线,进行2期测量,共计获取150个土壤气CO2组分浓度,计算了气体的相对活动强度; 收集了60件CO2气体样品,测试了其碳同位素组成。结果表明:岐山—马召断裂的气体活动强度(1.56~2.70)比固关—虢镇断裂的气体活动强度(1.73~1.75)大,且岐山—马召断裂上的CO2碳同位素组成比固关—虢镇断裂上的CO2更靠近深部物质端元。位于南段的岐山—马召断裂的地下构造连通性较好,断裂闭锁程度较低,而位于北段的固关—虢镇断裂气体活动性较弱,闭锁程度较高,未来发生地震的危险性较高。
Abstract:
The Longxian-Baoji Fault Zone is located in the northeast edge of the Qinghai-Tibet Block and belongs to the southernmost segment of the arc fault belt in the southwest edge of the Ordos Block.To compare the activity of the Qishan-Mazhao Fault in the south of the Longxian-Baoji Fault Zone with the activty of the Guguan-Guozhen Fault in the north,we study the geochemical features of the soil gas CO2 in the faults.Six survey profiles for surveying CO2 are deployed across the two faults and two periods of observation are carried out.We obtain 150 observed values of CO2 component concentrations.In addition,we collect 60 CO2 samples for stable carbon isotopic composition measurements.We find that the intensity(1.56-2.70)of CO2 activity in the Qishan-Mazhao Fault is greater than that(1.73-1.75)in the Guguan-Guozhen Fault.And the source of the CO2 in the Qishan-Mazhao Fault is closer to the end member of the deep materials.This suggests that the connectivity of the underground structures of the Qishan-Mazhao Fault is better and the fault's locking degree is lower.Meanwhile,the gas activity in the Guguan-Guozhen Fault is weaker and the fault's locking degree is higher.Thus,the earthquake risk in this fault zone is higher.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2021-11-23
基金项目:中国地震局地震预测开放基金(2021EFOF03)、陕西省自然科学基金(2022JQ-254)和中国地震局震情跟踪定向工作任务(2022010502、2021010309)联合资助.

更新日期/Last Update: 2022-05-20