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45篇 您的检索式:作者名="Nabelek"
    题名 作者 年代 出处 被引量
1青藏高原吉隆-鲁谷(Hi-Climb)层析成像与印藏碰撞的消减作用显示文摘利用中美合作Hi-Climb项目北段吉隆-鲁谷剖面的天然地震探测数据,拾取2004-2005年期间5级以上地震事件的P波与4级以上地震的Pn波震相的走时,通过多震相层析成像反演获得青藏高原腹地的地下500 km以上的P波速度扰动结构.结果表明雅江地区为北向倾斜的低速扰动,班公-怒江断裂下方存在向南俯冲并被印度板块俯冲挤压而回折的高速体,建立了印度板块在冈底斯地块下方拆沉并被雅江低速体穿越的构造样式.说明印度板块俯冲在到达班公-怒江缝合带之前已经开始消减,与拆沉位置对比发现,印度板块的前锋深部呈现多期多级次特征,并受到地幔热循环作用的影响.钱辉 姜枚 Chen Wangping John Nabelek Zhao Dapeng 赵磊 王亚军 2007地球物理学报2007,50,5:15
2喜马拉雅造山带的地壳上地幔结构--近震反射观测结果显示文摘2002—2005年完成了穿越喜马拉雅山的宽频地震探测,采用了沿剖面紧密排列的台站布置并获得了近震中的反射波资料,这对地壳和岩石圈内部速度界面的研究有重要意义。地震数据及研究结果表明,青藏高原的地震主要发生于上地壳范围内,高原莫霍面反射波的纵波 PmP 与横波 SmS 波至清晰可辨且有很强的能量,在跨越雅鲁藏布江时 PmP 和 SmS 均发生了错动,表现为北深南浅。在改则至鲁谷沿线所记录到的发生在拉萨地块的 Fw21事件的地震数据中,拉萨地块内部的莫霍面反射波,尤其是 SmS 波至非常清晰连续,地壳纵波平均速度为 V_p=6.3km/s,表明拉萨地块内部 Moho 面平坦、连续,不存在突起与错位。在此 Moho 面之前出现壳内较强反射界面,埋深45km 可能正是下地壳的顶界面。P208事件中 PmP 和 SmS 均清晰可见,然而在距震中450km 及其以远地段存在两个清晰的震相 P_(LT)及 S_(LT),并且其能量很强,可能是位于160km 深处的岩石圈底界面的反映。根据对近震资料的分析研究,本文建立了该地区的地壳上地幔的结构模型。姜枚 王有学 NABELEK John 钱辉 王亚军 刘因 张立树 赵磊 2008岩石学报2008,24,7:4
3Role of obfique convergence in the active deformation of the Himalayas and southern Tibet plateau 显示文摘Mc Caffery R Nabelek J 1998Geology1998,26,:1
4General equations for modeling fluid/rock interaction using trace elements and isotope 显示文摘 1987Geochim et Cosmochim Acta1987,51,:1
5The Tangshan earthquake sequence and its implications for the evolution of the North China basin显示文摘Nabelek J Chen W P Ye H 1987J GeophvsRes1987,92,12:1
6Seismogenic strike-slip faulting and the development of the North China Basin显示文摘Chen W P Nabelek J 1988Tectonics1988,7,:1
7Heat and fluid flow in contact metamorphic aureoles with layered and transient permeability, with application to the Notch Peak aureole, Utah显示文摘CUI X J NABELEK P I LIU M 2001J Geophys Res2001,106,:1
8The role of H2O in rapid emplacement and crystallization of granite peg- matites: Resolving the paradox of large crystals in highly un- dercooled melts显示文摘Nabelek P I Whittington A C- Sirbescu M C 2009Contributions to Mineralogy and Petrolo-gy2009,160,:1
9Evidence form earthquake data for a partially molten crustal layer in southern Tibet 显示文摘Kind R Ni J Zhao W Wu J Yuan X Zhao L Sandvol E Reese C Nabelek J Hearn T 1996Science1996,274,:1
10Acce-ptablenoise level as a predictor of hearing aid use 显示文摘Nabelek AK Freyaldenhoven MC Tampas JW 2006J Am Aead Audiol2006,17,9:1
11General equations for modeling fluid/rock interaction using trace elements and isotopes显示文摘NABELEK P I 1987Geochim Cosmochim Acta1987,51,:1
12Role of oblique convergence in the active deformation of the Himalayas and Southern Tibet Plateau 显示文摘MCCAFFREY R NABELEK J 1998Geology1998,26,8:1
13Seismogenic strike-slip faulting and the development of the North China Basin 显示文摘Chen W P Nabelek J 1988Tectonics1988,7,5:1
14Heat and fluid flow in contact metamorphic aureoles with layered and transient permeability, with application to the Notch Peak aureole, Utah显示文摘CUI X J NABELEK P I LIU M 2001J Geophy Res2001,106,:1
15Accepta ble noise level as a predictor of hearing aid use显示文摘Nabelek AK Freyaldenhoven MC Tampas JW 2006J Am Acad Audiol2006,17,:1
16Toleration of Background Noises :Relationship with Patterns of Hearing Aid Use by Elderly Persons 显示文摘Anna Nabelek Frances Tucker Tomasz Letowski 1991Journal of Speech- Language-Hearing Research1991,,34:1
17Toleration of back- ground noises: Relationship with patterns of hearing aid use by elderly persons 显示文摘Nabelek AK Tucker FM Leowski TR 1991J Speech Hear Res1991,34,:1
18Toleration of background noises:Relationship with patterns of hearing aid use by elderly persons 显示文摘Nabelek Tucker Letowski 1991Journal of Speech Langnage and Hearing Restearch1991,1991,34:1
19Reverberant overlap-and self-masking in consonant identification 显示文摘Nabelek A K Letowski T R Tucker F M 1989The Journal of the Acoustical Society of America1989,86,:1
20Comparison of speech perception in background noise with acceptance of background in aided and unaided conditions 显示文摘Nabelek AK Tampas JW Burchfield SB 2004J Speech Lang Hear Res2004,47,:1
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