STUDY ON CHARACTERISTICS OF CO2 ANOMALIES IN DIFFERENT DEPTHS IN BURIED FAULTS
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摘要: 本文对比研究了华北北部隐伏活动的唐山断裂和夏垫断裂以及隐伏不活动的香河-皇庄断裂上0.5m和2.0m深处的CO2异常特征,并初步讨论了CO2异常机理及不同深度CO2异常特征在判断隐伏断裂位置及其活动性中的应用。0.5m深处的CO2在隐伏活动断裂和隐伏不活动断裂上均有异常;而2.0m深处CO2在隐伏活动断裂上异常显著,在隐伏不活动断裂上则没有异常。2.0m深处CO2异常范围比0.5m深处CO2异常范围小得多。认为0.5m深处CO2主要来源于生物作用,而2.0m深处CO2则主要来源于碳酸盐岩的破释气。Abstract: In this paper, foe Authors study the characteristics of CO2 anomalies in 0.5m and 2.0m depth in Tangshan and Xiadian buried active faults and Xianhe-Huangzhuang buried inact ive fault in the northern part of North China, and preliminarily discuss the mechanism of CO, anomaly and applications of CO2 anomalous features in different depths in determining locations and activities of the buried faults. CO2, contents in 0.5m depth show distinct anomalies both in the buried active and inactive faults, however, CO2 contents in 2.0m depth show notable anomalies in the buried active faults but don't show anomaly in the buried inactive fault. The width of CO2 anomaly estension in 2.0m depth is much more narrower than that in 0.5m depth. It is suggested that CO2 in 0.5m depth is mainly originated from biogenic agency while CO2 in 2.0m depth is primarily derived from degassing in the processes of carbonte rock ruptures caused by fault movement.
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Key words:
- buried fault /
- fault position /
- CO2 anomaly in different depth /
- mechanism of anmmaly
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[1] 1 国家地震局《一九七六年唐山地震》编辑组.一九七六年唐山地震.北京:地震出版社. 1982.
2 向宏发,等.三河-平谷8级地震区的构造背景与大震重复性研究.地震地质. 1988. 10 (1):15-28
3 邵学钟,等.京津唐地区地震转换波测深结果.地震地质. 1980. 2 (2):11-20
4 林元武,程盛华.断层气CO2快速测定法及其在地震研究中的应用.地震. 1993. 65-67
5 惠荣耀,等.准噶尔盆地马庄气藏-I.地球化学特征.中国科学(B辑). 1991. (12),1304-1312
6 Koyama. T., Gaseous metabolism in lake sediments and paddy soils and the production of atmosperic methane and hydrogen. J. Geophys. Res.. 1963. 68 (810),3971-3973.
7 杨新华等.云南大理岩破坏过程中的气体发散现象.地震. 1984. (5),16-20 -

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