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53篇 您的检索式:作者名="Saleeby"
    题名 作者 年代 出处 被引量
1变泥质岩的深熔作用与具铈(Ce)负异常熔体的成因显示文摘对美国加州南Sierra Nevada岩基中一个典型的中生代变质表壳岩及其混合岩带进行了详细的野外观察和元素地球化学研究。研究发现:在持久(约为150Ma)的花岗岩侵位作用下,早白垩世变泥质岩发生达角闪岩相的中高级变质作用和部分熔融,导致Isabella混合岩的形成;浅色体具有和变泥质岩及混合岩近平行的REE分布模式,但浅色体的LREE含量相对较低;和变泥质岩相似,混合岩中的浅色体具有显著的Ce负异常。野外观测、岩相观察及元素地球化学特征表明,浅色体显著的Ce负异常是继承了原岩的Ce负异常特征,而不是由于副矿物(磷灰石、独居石或锆石)的差异溶解或结晶分异作用造成的。早白垩世变泥质岩(浅色体的原岩)主要由泥质及沙质海相沉积物组成,局部夹基性火山灰和火山碎屑,形成于与大陆岛弧密切相关的浅海环境。原岩的Ce负异常反映了较还原的浅海沉积环境。具有Ce负异常浅色体的产出表明,如果俯冲带上的沉积岩在俯冲过程中发生部分熔融作用并且所产生的熔体参与大洋型岛弧岩浆作用,最终可以导致具有Ce异常的基性岩浆生成。曾令森 Mihai DUCEA Jason SALEEBY 2005岩石矿物学杂志2005,24,5:14
2大型花岗岩基形成和演化的深部动力学过程:滴水构造、钾质火山作用与地表地质过程显示文摘以美国内华达山脉复合岩基为例,系统评述了与大型花岗岩基的形成、演化相关的深部地球动力学过程及构造地貌学响应。在大陆岛弧环境下,基性岩浆的底侵作用促使下地壳发生角闪岩脱水部分熔融,在岩基根部形成高密度的石榴辉石岩,岩基根部最终发生重力失稳,形成滴水构造;在地貌上反映为滴水构造对应区域的沉降和相应的张性构造,在岩浆作用上则表现为软流圈地幔上涌和残余富集岩石圈地幔的低程度部分熔融,形成钾质火山岩。这种高度动态的深部动力学过程是维持大型花岗岩基地区较高高程或促使这些区域高程骤然增加的重要因素。曾令森 刘静 Jason B Saleeby 2006地质通报2006,25,11:12
3H1N1 influenza in pregnancy: cause for concern 显示文摘Saleeby E Chapman J Morse J 2009Obstet Gynecol2009,114,4:1
4U/Pb zircon, strontium, and oxygen isotopic and geochronological study of the southernmost Sierra Nevada batholith, California显示文摘Saleeby J B Sams D B Kisder R W 1987Journal of Geophysical Research1987,92,10:1
5Thermobarometry of Cretaceous rocks of the Tehachapi Mountains, California: Plutonism and metamorphism in deep levels of the Sierra Nevada batholith显示文摘Pickett D A Saleeby J B 1993Journal of Geophysical Research1993,98,:1
6HIM influenza in pregnancy:cause for concern显示文摘Saleeby E Chapman J Morse J 2009Obstet Gynecol2009,114,4:1
7Topographic response to mantle lithosphere removal in the southwest Sierra Nevada,California显示文摘Saleeby J B Foster Z A 2004Geology2004,32,:1
8Respiratory syncytial virus load predicts disease severity in previously healthy infants显示文摘DeVincenzo JP El Saleeby CM Bush AJ 2005J Infect Dis2005,191,11:1
9Respiratory syncytial virus load predicts disease severity in previously healthy infants显示文摘De Vincenzo JP El Saleeby CM Bush AJ 2005J Infect Dis2005,191,11:1
10Coupling of anatectic reactions and dissolution of accessory phases and the Sr and Nd isotope systematics of anatectic melts from a metasedimentary source显示文摘Zeng L Asimow P Saleeby J B 2005Geochimica et Cosmochimica Acta2005,69,:1
11All pain is not the same: An overview of neuropathic pain in the elderly显示文摘Martin C M Saleeby L G 2007Journal of the American Society of Consultant Pharmacists2007,22,4:1
12Nd isotope disequilibrium during crustal anatexis: A record from the Goat Ranch migmatite complex, southern Sierra Nevada batholith, California显示文摘Zeng L Saleeby J B Asimow P 2005Geology2005,33,:1
13H1N1 influenza in pregnancy: cause for concern显示文摘Saleeby E Saleeby E Chapman J 2009Obstet Gynecol2009,114,4:1
14Nd,Sr and Pb isotopic characteristics of Cretaceous intrusive rocks from deep levels of the Sierra Nevada batholith Tehachapi Mountains California显示文摘Pickett D A Saleeby J B 1994Contributions to Mineralogy and Petrology1994,118,:1
15Ophicalcites and related rocks of the Kings-Kaweah ophiolite belt,Southwest Sierra Nevada foothills显示文摘Saleeby J Sharp W D 1977American Geophysical Union1977,58,12:1
16Nd isotope disequilibrium during crustal anatexis:A record from the Goat Ranch migmatite complex southern Sierra Nevada batholith (SNB) California显示文摘Zeng L Saleeby J B Asimow P 2005Geology2005,33,:1
17Geochemical characteristics of crustal anatexis during the formation of migmatite at the Southern Sierra Nevada,California显示文摘Zeng L Saleeby J B Ducea M 2005Contributions to Mineralogy and Petrology2005,150,4:1
18Respiratory syncytial virus load,viral dynamics,and disease severity in previously healthy naturally infected children显示文摘E1 Saleeby CM Bush AJ Harrison LM 0,,07:1
19The non-equilibrium landscape of the southern Sierra Nevada,California显示文摘Clark M K Maheo G Saleeby J B 2005GSA Today2005,15,9:1
20Geochemical characteristics of crustal anatexis during the formation of migmatite at the Southern Sierra Nevada, California 显示文摘Zeng L Saleeby J B Ducea M 2005Contributions to Mineralogy and Petrology2005,150,:1
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