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从水热膨胀观点管窥盆地超压
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作者 陈瑞军 王继革 +1 位作者 李嫄嫄 边宗斌 《吉林大学学报(地球科学版)》 EI CAS CSCD 北大核心 2012年第S3期44-53,共10页
从水热膨胀的观点,依据板桥凹陷地质条件,应用水热膨胀压表达式,计算分析该凹陷不同深度地层温度、压力及其分布特征,再通过国内部分盆地及巴库群岛地区的地层压力的勘查成果对比,认为:地层压力异常起源于盆地下部,对于板桥凹陷来说形... 从水热膨胀的观点,依据板桥凹陷地质条件,应用水热膨胀压表达式,计算分析该凹陷不同深度地层温度、压力及其分布特征,再通过国内部分盆地及巴库群岛地区的地层压力的勘查成果对比,认为:地层压力异常起源于盆地下部,对于板桥凹陷来说形成深度为7 400~8 500 m、温度为271.10~309.6℃;温度是控制压力变化方向的主要因素;盆地地层圈闭是次生圈闭,与深度无关;通过应用水热膨胀压表达式,对惠民凹陷的临南洼陷中构造、地层压力及地温演化的关系分析,认为地层负压是在地层圈闭后地温下降水凉收缩产生的。这些可为地层压力成因解释、油气成藏与地热成储研究及钻前压力预测提供帮助,为深部资源的寻找提供思路。 展开更多
关键词 地热能 异常地层压力 地层圈闭 压力分带 泥岩底辟 板桥凹陷
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Analysis on Characteristics of Focal Mechanisms for the M_S7.3 Yutian Earthquake Sequence of February 12,2014
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作者 Li Jin Wang Qiong 《Earthquake Research in China》 CSCD 2015年第4期527-538,共12页
The paper inverts the focal mechanism solutions of the Yutian M_S7. 3 main shock,foreshocks and M_S≥3. 5 aftershocks by using the CAP method,based on the broadband waveforms recorded by the Xinjiang and Tibet Digital... The paper inverts the focal mechanism solutions of the Yutian M_S7. 3 main shock,foreshocks and M_S≥3. 5 aftershocks by using the CAP method,based on the broadband waveforms recorded by the Xinjiang and Tibet Digital Seismic Networks. The results show that the M_S7. 3 strong earthquake is of strike-slip type with a normal faulting component,and combined with the analysis of focal structure and the aftershock distribution,the nodal plane I with strike 241°,dip 90° and rake- 22° is considered to be the seismogenic fault plane of the main shock. The direction of P-axis for the main shock is 194°,close to the near NS direction of the principal stress P-axis of historical strong earthquakes in this region. The focal mechanism solution of the M_S5. 4 foreshock has a good consistency with that of the main shock. Among the 18 aftershocks,10 are of strike-slip type,6 are of normal faulting type and 2 are of thrust type. 70% of the aftershocks in the sequence have a focal mechanism with P-axis in the near-NS direction. The focal depths of this M_S7. 3 earthquake sequences are distributed in the range of 5km- 28 km,with the majority in the depth range of 15km- 20 km,slightly deeper than the depth of 10 km of the main shock as calculated. 展开更多
关键词 Yutian MS7.3 earthquake Focal mechanism CAP method AFTERSHOCK
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Controlling Thermal Conductivity of Few-Layer Graphene Nanoribbons by Using the Transversal Pressure
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作者 钟伟荣 杨明明 +1 位作者 张茂平 艾保全 《Communications in Theoretical Physics》 SCIE CAS CSCD 2013年第9期353-356,共4页
We study the thermal transport of few-layer graphene nanoribbons in the presence of the transversal pressure by using molecular dynamics simulations. It is reported that the pressure can improve the thermal conductivi... We study the thermal transport of few-layer graphene nanoribbons in the presence of the transversal pressure by using molecular dynamics simulations. It is reported that the pressure can improve the thermal conductivity of few-layer graphene nanoribbons. This improvement can reach 37.5% in the low temperature region. The pressure dependence of thermal conductivity is also investigated for different length, width and thickness of few-layer graphene. Our results provide an alternative option to tuning thermal conductivity of few-layer graphene nanoribbons, b-arthermore, it maybe indicate a so-called pressure-thermM effect in nanomaterials. 展开更多
关键词 thermal conductivity GRAPHENE molecular dynamics simulation PRESSURE
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